The Issue The issue to be determined by this Order is whether the Request for Administrative Hearing filed by Petitioner with the Department of Environmental Protection (“DEP”) on February 15, 2013, was timely1/ and, if not, whether the application of the doctrine of equitable tolling would serve to relieve Petitioner of the consequences of having failed to file a petition for hearing within the time allotted by applicable notice provisions.
Findings Of Fact The Parties Petitioner, SRQUS, LLC, is an active Florida, limited- liability corporation, and is the owner of submerged lands and adjacent upland property contiguous to Sarasota Bay. Petitioner is a closely held entity, the only members being Achim and Erika Ginsberg-Klemmt. Respondent, Department of Environmental Protection, is an agency of the State of Florida having jurisdiction for permitting Municipal Separate Storm Sewer Systems (MS4), including duties as a federally-approved state program for the implementation of the Federal National Pollutant Discharge Elimination System (NPDES) Program, pursuant to authority conferred under section 403.0885, Florida Statutes. Respondents, Sarasota County, City of Sarasota, City of Venice, Town of Longboat Key, and Department of Transportation (“DOT”) (collectively the “Applicants”) are responsible for certain existing stormwater point-source discharges to waters of the state from those portions of MS4 facilities owned or operated by one or more of the individual Applicants. The DEP issued a notice of proposed agency action to issue a renewal of an existing MS4 Permit to the Applicants. On January 30, 2013, Sarasota County arranged for the notice to be published in the Sarasota Herald-Tribune, which is a newspaper of general circulation in Sarasota County. The notice provided as follows: STATE OF FLORIDA DEPARTMENT OF ENVIRONMENTAL PROTECTION NOTICE OF INTENT TO ISSUE PERMIT AND REQUEST FOR ADMINISTRATIVE HEARING The Department of Environmental Protection gives notice of its intent to issue a permit to Sarasota County, 1660 Ringling Boulevard, Sarasota, Florida 34236 within its jurisdiction and including the following co- permittees: Florida Department of Transportation District One, Town of Longboat Key, City of North Port, City of Sarasota, and City of Venice, for renewal of a Municipal Separate Storm Sewer System [MS4] permit. Any person whose substantial interests are affected by the proposed permitting decision of the Department may petition for an administrative hearing in accordance with Sections 120.569 and 120.57 of the Florida Statutes (F.S.). The petition must contain the information set forth below and must be filed (received) in the Department of Environmental Protection, Office of General Counsel, Mail Station 35, 3900 Commonwealth Boulevard, Tallahassee, Florida 32399-3000. Petitions must be filed within fourteen days of publication of this public notice or within fourteen days of receipt of the notice of intent, whichever occurs first. A petitioner must mail a copy of the petition to the applicant at the address indicated above, at the time of filing. The failure of any person to file a petition [or a request for mediation, as discussed below] within the appropriate time period shall constitute a waiver of that person?s right to request an administrative determination (hearing) under Sections 120.569 and 120.57, F.S., or to intervene in this proceeding and participate as a party to it. Any subsequent intervention will be only at the discretion of the presiding officer upon the filing of a motion in compliance with Rule 28-5.207 of the Florida Administrative Code. A petition must contain the following information: The name, address and telephone number of each petitioner, the Department Permit Number and the county in which the MS4 is located; A statement of how and when each petitioner received notice of the Department?s action; A statement of how each petitioner?s substantial interests are affected by the Department?s action; A statement of the material facts disputed by the petitioner, if any; A statement of facts that the petitioner contends warrant reversal or modification of the Department?s action; A statement of which rules or statutes the petitioner contends require reversal or modification of the Department?s action; and A statement of the relief sought by the petitioner, stating precisely the action that the petitioner wants the Department to take. Because the administrative hearing process is designed to formulate final agency action, the filing of a petition means that the final action of the Department may be different from the position taken by it in the notice of intent. Persons whose substantial interests will be affected by any such final decision of the Department on the permit revision have the right to petition to become a party to the proceeding, in accordance with the requirements set forth above. Mediation under Section 120.573, F.S. is not available for this proceeding. The permit application file and supporting data are available for public inspection during normal business hours, 8:00 a.m. to 5:00 p.m., Monday through Friday, except legal holidays, at Department of Environmental Protection, NPDES Stormwater Section, 2600 Blair Stone Rd. Room 560, Tallahassee, Florida 32399-2400, phone number (850) 245-8430. Date of pub. January 30, 2013. Because a portion of the Town of Longboat Key extends into Manatee County, the Town of Longboat Key arranged for the notice to be published in the Bradenton Herald, which is a newspaper of general circulation in Manatee County. The notice was published on February 4, 2013. The substance of the notice, except for the date of publication, was identical to that published in the Sarasota Herald-Tribune. Neither Petitioner, nor its representatives, saw either of the published notices prior to the filing of the Petition. On or about February 8, 2012, as a result of the filing of a pre-hearing stipulation in related litigation involving an Environmental Resource Permit (“ERP”) issued by the Southwest Florida Water Management District (“SWFWMD”), Petitioner became aware of the existence of the MS4 Permit. Erika Ginsberg-Klemmt obtained a copy of the permit online, and on February 12, 2013, sent an e-mail to employees of the DEP Ft. Myers? office expressing her general concern with water quality from the disputed stormwater outfall. She expressed her belief that Sarasota County was in violation of the existing MS4 permit, and requested that the recipients of her e-mail “[p]lease be so kind as to look into this matter and let us know what could be done to prevent this unacceptable condition to continue unchecked like it did in the past.” The e-mail did not request any information regarding the MS4 Permit renewal application, nor did it request any information regarding notices or deadlines related to the application. On February 13, 2013, Christopher Wright, a consultant for Petitioner, called the DEP to gather information and do some “legwork” related to Petitioner?s challenge to the SWFWMD?s ERP. The purpose of the call was to determine if information submitted to the DEP in conjunction with the MS4 application, particularly drainage basin maps, could have been of use in the SWFWMD litigation. Mr. Wright spoke with DEP employee, Heather Ritchie, regarding the drainage basin maps that had been submitted to the DEP. During the course of their discussion, Ms. Ritchie advised Mr. Wright that a Notice of Intent to issue the MS4 Permit had been issued by the DEP. However, Ms. Ritchie did not know when Sarasota County had published the notice or when the deadline for challenging the proposed agency action was to run. In short, Ms. Ritchie expressed to Mr. Wright that “she didn?t know what the status of things were.” The discussion then went back to the primary substance of the call, which was watersheds and discharge points. Ms. Ritchie agreed to provide Mr. Wright with an electronic copy of a drainage map from the MS4 Permit file. At 12:43 p.m., on February 13, 2013, Ms. Ritchie sent a map to Mr. Wright via e-mail, and indicated that “[i]f you have additional questions or comments, you may call or e-mail me.” Later on the afternoon of February 13, 2013, Mr. Wright decided that he should ask Ms. Ritchie for a copy of the Notice of Intent. At 5:59 p.m., on February 13, 2013, after the close of business for the day, Mr. Wright wrote to Ms. Ritchie thanking her for her “rapid response to my inquiry today,” and providing her with comments on various basin areas and discharge structures. Mr. Wright concluded his e-mail by stating that “at this time I would also like to request a copy of the Notice of Intent to Issue the MS4 Permit.” The next morning, February 14, 2013, Ms. Ritchie provided Mr. Wright with the Notice of Intent to Issue the MS4 Permit as requested. Later that morning, Mr. Wright inquired as to the time for filing a challenge to the permit. Ms. Ritchie replied at 2:34 p.m. that afternoon that the MS4 Permit “was publicly noticed by the county on January 30th with a 14 day window. The window closed yesterday.” There is no evidence that Ms. Ritchie had any specific information as to the date of publication or the deadline for filing a challenge prior to that communication with Mr. Wright. Petitioner filed the Petition on February 15, 2013. The disputes identified in the Petition were directed exclusively at a 46-acre drainage basin in downtown Sarasota, and a related discharge structure that discharges stormwater from the basin to Sarasota Bay just south of the intersection of U.S. Highway 41 and Fruitville Road. The disputed basin and discharge point are located in Sarasota County.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that Respondent, Department of Environmental Protection, issue a final order dismissing Petitioner?s Request for Hearing and Amended Petition for FLS000004-004 on the ground that the Petition was not timely filed. DONE AND ENTERED this 18th day of October, 2013, in Tallahassee, Leon County, Florida. S E. GARY EARLY Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 18th day of October, 2013.
The Issue The issues in this case are: (1) whether proposals by Richard and Mildred Olson to widen an existing bridge (designated Bridge 1) and construct two new pedestrian bridges (designated Bridges 2 and 4) across Bessey Creek in Martin County, Florida, qualify for the Noticed General Permit established by Rule 62-341.475; and (2) whether Petitioner participated in this proceeding for an improper purpose under Section 120.595(1). (Citations to sections are to the 2000 codification of Florida Statutes. Rule citations are to the current Florida Administrative Code.)
Findings Of Fact Richard and Mildred Olson own property in Rustic Hills Phase III in Martin County, Florida. The Olsons own lots 191, 192, 195, 212, 213, and 214. Each lot is approximately two acres in size. The Olson home is on lot 213, and a rental home is on lot 195. On their property, the Olsons raise miniature goats, guinea hens, and peacocks; they also have ducks, geese, chickens, and dogs. Bessey Creek winds through Rustic Hills and the Olsons' lots. The Olsons propose to use DEP's NGP for Minor Activities established by adoption of Rule 62-341.475 to widen one existing bridge and construct two others for access to their property across Bessey Creek. Bessey Creek is a tributary of the St. Lucie River, through man-made Canal 23. Navigating upstream on Bessey Creek, a boat would have to pass under the Murphy Road Bridge, which is 9 feet, one inch above mean high water (MHW), just before reaching the first of the four bridges involved in this case, Bridge 1. Bridge 1 is a steel span bridge (with no pilings in the water) that connects two portions of lot 191, which is split by the creek. The Olsons propose to widen existing Bridge 1. It is not clear from the evidence whether pilings will be required to widen Bridge 1. But it seems clear that a centerline stream clearance (horizontal width) of 16 feet and a bridge height above mean high water (MHW) (vertical clearance) of 9 feet will be maintained. Proposed pedestrian Bridge 2 is the next bridge upstream, at a point where the creek is only approximately 24 feet wide from MHW to MHW. It is designed to be a 192 square foot piling-supported bridge, with an 8-foot wide by 24-foot long walkway. To support Bridge 2, sets of pilings will placed in the creek bed so as to maintain a centerline stream clearance of 16 feet. The proposed vertical clearance for Bridge 2 is 8 feet above MHW. Existing Bridge 3, the next upstream, is at a point where the creek is approximately 35 feet wide from MHW to MHW. Bridge 3 is a wooden bridge approximately 25 years old. It connects lots 192 and 193 to lot 191. The Olsons use existing Bridge 3 on a daily basis. Bridge 3 was built to span the creek; later, two sets of wooden piles were added. There is a centerline stream clearance of 13 feet between the piles. Vertical clearance is 8 feet above MHW. Proposed pedestrian Bridge 4, the farthest upstream, is designed in the same manner as proposed pedestrian Bridge 2. It is located at a point where the creek is approximately 35 feet wide from MHW to MHW. Bridge 4 will connect lots 195 and 212. Navigability Proposed pedestrian Bridges 2 and 4 are designed to have the same 8-foot vertical clearance as existing Bridge 3; they are designed to have three feet more horizontal clearance than existing Bridge 3. Neither they nor widened Bridge 1 will restrict navigation as much as existing structures, natural conditions (including numerous fallen trees, underwater snags and low, overhanging vegetation), and docked boats. The United States Coast Guard and the Florida Fish and Wildlife Conservation Commission (FFWC) concur that the bridges would not have any deleterious effect on the navigation in this area of Bessey Creek. While not specifically alleging impedance of navigation, Petitioner alleged that existing Bridges 1 and 3 are lower than measured by the Olsons' environmental consultant. But there was no evidence to support such a finding. Meanwhile, the Olsons' consultant explained how he determined the vertical clearance of those bridges above MHW by measurements adjusted for MHW using NOAA tide charts. Even if existing Bridges 1 and 3 had less vertical clearance than determined by the Olsons' consultant, Bridges 2 and 4 are designed to have the same vertical clearance as the consultant determined Bridge 3 to have. For that reason, even if the consultant's determinations were incorrect, the vertical clearances of Bridges 2 and 4 are designed to be the same as the vertical clearance of Bridge 3, and the vertical clearance of Bridges 2 and 4 will not impede navigation any more than Bridge 3. Flooding Bessey Creek is a typical tidal creek. It has low volume and low velocity. Being influenced by tidal ebb and flow, its flow is not continuously downstream except during and just after times of high precipitation, such as hurricanes. Under these conditions, build-up of debris around pilings of these bridges would not be expected, and none was observed around at the existing bridges. The chances of vegetation or organic matter building up over time in the area of these bridges to create a beaver dam effect and cause flooding are small. The proposed new pedestrian bridges have four pilings, which is typically less than a single-family dock. The pilings of a single-family dock are closer to the shoreline and, particularly with a boat alongside, would have more potential to trap debris and cause flooding than the proposed bridges. The same can be said of the fallen trees and low, overhanging vegetation existing under natural conditions in Bessey Creek. The proposed bridges are not expected to have an adverse impact of a significant nature with respect to off-site flooding. Petitioner did not present any expert testimony regarding allegations of off-site flooding potential. Dan White testified as a lay person that flooding occurs in the area during times of high precipitation and that Petitioner was concerned that the proposed bridges would exacerbate those conditions. But, while the evidence was clear that flooding is a condition to be expected under certain conditions in low-lying areas like Rustic Hills Phase III, White failed to make any causal connection between existing periodic flooding and the bridges, existing or proposed. Improper Purpose Petitioner's request for hearing, by letter dated November 16, 2000, thanked DEP for "this opportunity to contest the granting of a Noticed General Permit to the Olson's [sic]" and also requested "an Administrative Review to ensure your department has all the information needed to make a fair decision regarding this matter." It also requested: "Since we are a small community, I hope the Department will review this petition in light of the author's lack of familiarity with the specific form and format used by the environmental consultants and those who work with you on a regular basis." Petitioner "respectfully submit[ted] the following information which is required to dispute the Department's actions and to request an Administrative hearing if necessary." In response to Petitioner's letter, DEP referred the matter to DOAH. Apparently, Petitioner (and the other parties) did not receive a copy of the Initial Order. Petitioner, which was not represented by counsel at the time, failed to comply with the Amended Initial Order entered on March 23, 2001. But apparently neither did the Olsons, who also were not represented by counsel at the time, or DEP, which was. The Olsons complained by letter filed April 26, 2001, that Petitioner had not contacted them. But there was no indication or evidence that, up to that point in time, the Olsons attempted to contact Petitioner or DEP, or that DEP attempted to contact Petitioner or the Olsons, in response to the Amended Initial Order. The Joint Response to Initial Order filed by the Olsons and DEP on May 1, 2001, recited that Petitioner's contact person-of-record, Treasurer Jim Fyfe, "no longer was associated with Rustic Hills" and that Petitioner's President, Dan White, was "out of town and could not be reached." Based on the Joint Response to Initial Order filed by DEP and the Olson's, final hearing was scheduled for May 24, 2001. The Order of Pre-Hearing Instructions entered along with the Notice of Hearing on May 3, 2001, required that the parties exchange witness lists and copies of exhibits and file their witness lists by May 14, 2001. Petitioner complied with the requirement to file a witness list and also included a list of exhibits. There was no indication or evidence that Petitioner did not exchange exhibits as well. The Order of Pre-Hearing Instructions also required: "No later than May 18, 2001, the parties shall confer with each other to determine whether this cause can be amicably resolved." When the Olsons' environmental consultant, Bruce Jerner, went to Dan White's home on May 14, 2001, to provide him a copy of the Olsons' exhibits, he invited White to discuss settlement in accordance with the Order of Pre-Hearing Instructions. White responded to the effect that, even if Petitioner did not have a strong case, Petitioner preferred to go to hearing, and White did not want to mediate or discuss settlement with Jerner. At that point, Jerner indicated that he would be sending White a letter confirming the Olsons' attempt to comply with the Order of Pre-Hearing Instructions. The letter dated the next day requested "an informal conference to determine whether the above referenced case can be amicably resolved and avoid hearing proceedings." Significantly, there was no indication or evidence that DEP complied with the Order of Pre-Hearing Instructions in any respect. It appears that DEP distanced itself from the dispute between Petitioner and the Olsons, preferring to allow them to settle or litigate as they saw fit. In view of DEP's noncompliance, DEP at least certainly may not rely on Petitioner's noncompliance as a ground for an award of attorney fees and costs. In addition, while DEP's noncompliance does not excuse Petitioner from complying, it helps put Petitioner's actions in context and is relevant on the question whether Petitioner's noncompliance was evidence of improper purpose. In this regard, White testified to his belief that he had complied with all ALJ orders but did not "know why I would be obligated to respond to the consultant for Mr. Olson with regard to hearing or any other matters." While DEP and the Olsons in part cite Petitioner's failure to follow prehearing procedures, they primarily rely on the weakness of Petitioner's presentation at final hearing and posthearing efforts as evidence of improper purpose. But this evidence must be evaluated along with other factors resulting in the weakness of Petitioner's case. Not only did White misinterpret the Order of Pre- Hearing Instructions, the evidence indicated that he was unfamiliar with the administrative process in general and also was confused about the difference between the administrative hearing scheduled for May 24, 2001, and the County permitting proceedings on the bridges which also were on-going. White indicated repeatedly during final hearing that he and Petitioner had just recently learned more about distinctions between the administrative and County permit proceedings. As a result, White was beginning to recognize that several issues Petitioner had attempted to raise in this administrative proceeding may be relevant to on-going County permit proceedings but not this administrative proceeding. When it was established and explained at final hearing that DEP had no jurisdiction to require demolition or repair of existing bridges in this proceeding, White agreed to withdraw that part of Petitioner's request for relief. When it was established and explained that issues Petitioner raised relating to the "public interest" test under Rules Chapter 21-18 were premature, White did not object to those issues being dropped. Later, when Petitioner attempted to raise water quality issues relating to excrement from Olson livestock crossing these bridges, and it was ruled that no such issue was raised in Petitioner's request for hearing, White accepted the ruling. Final hearing proceeded on the only remaining issue specifically raised by Petitioner (alleged off-site flooding) (together with navigability--an issue addressed in the Olsons' presentation but not raised in Petitioner's request for hearing). To use White's words, Petitioner did not "have a very sophisticated presentation." Petitioner had no expert testimony, and White's lay testimony did not make a causal connection between flooding and the bridges. After the presentation of evidence, Petitioner did not withdraw its request for hearing in view of the evidence presented; but, in fairness, neither was Petitioner asked to do so. Petitioner did not order a Transcript, or a copy after the Olsons ordered a Transcript, and did not file a PRO. It is fairly clear from the evidence that Petitioner did not participate in this proceeding primarily to cause unnecessary delay. Even if Petitioner had never requested a hearing, the Olsons did not have all of the authorizations required of DEP for their proposals. In addition, County permits apparently also are required. It seems reasonably clear that, had Petitioner retained a competent expert to evaluate its case, the expert probably would have advised Petitioner that it would not be able to make a causal connection between flooding and the bridges. Had Petitioner retained counsel prior to final hearing, counsel probably would have advised Petitioner not to proceed with its request for hearing because, without a causal connection between flooding and the bridges, Petitioner would not be able to prevail. But there was no indication or evidence that Petitioner had and disregarded the benefit of professional advice. Under the totality of these circumstances, it was not proven that Petitioner's participation in this proceeding was for an improper purpose--i.e., primarily to harass or to cause unnecessary delay or for frivolous purpose or to needlessly increase the cost of licensing or securing the approval of the Olsons' applications.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is RECOMMENDED that DEP enter a final order: denying Petitioner's challenge to the propriety of the Olsons' use of the NGP for minor activities for their proposals; authorizing the Olsons to use the NGP for their proposals (DEP File Nos. 43- 0137548-002 and 43-0158123-002) subject to the design criteria limitations and other conditions in the applicable general permit rules; and denying the Motion for Attorney's Fees from Petitioner under Section 120.595(1). Jurisdiction is reserved to enter a final order on the part of the Motion for Attorney's Fees seeking sanctions under Section 120.569(2)(e). DONE AND ENTERED this 30th day of July, 2001, in Tallahassee, Leon County, Florida. J. LAWRENCE JOHNSTON Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 www.doah.state.fl.us Filed with the Clerk of the Division of Administrative Hearings this 30th day of July, 2001. COPIES FURNISHED: Francine M. Ffolkes, Esquire Department of Environmental Protection 3900 Commonwealth Boulevard The Douglas Building, Mail Station 35 Tallahassee, Florida 32399-3000 Dan White, President Rustic Phase III Property Owners Association 3337 Southwest Bessey Creek Trail Palm City, Florida 34990 Tim Morell, Esquire 1933 Tom-a-Toe Road Lantana, Florida 33426 Elizabeth P. Bonan, Esquire Cornett, Googe, Ross & Earle, P.A. 401 East Osceola Street Stuart, Florida 32991 Kathy C. Carter, Agency Clerk Office of General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Station 35 Tallahassee, Florida 32399-3000 Teri L. Donaldson, General Counsel Department of Environmental Protection 3900 Commonwealth Boulevard, Mail Station 35 Tallahassee, Florida 32399-3000 David B. Struhs, Secretary Department of Environmental Protection 3900 Commonwealth Boulevard The Douglas Building Tallahassee, Florida 32399-3000
The Issue The issues for disposition are whether BJM Associates, Inc. is required to apply for and obtain a drainage connection permit pursuant to rule 14-86, Florida Administrative Code, and if so, whether BJM Associates, Inc., has failed to obtain that permit.
Findings Of Fact Respondent, BJM Associates, Inc. (BJM) is the owner and developer of Rosetta Villas Subdivision, located in Orange County, Florida, (Respondent’s prehearing Statement) Petitioner, Department of Transportation (D0T) purchased an adjacent parcel, including a retention pond, “Pond A”, in 1991, in anticipation of a road-improvement or extension project for Maitland Boulevard. The pond was purchased from Rose Industrial Park, a permitted development also adjacent to the pond. Rosetta Villas Subdivision received Orange County subdivision approval in 1986 and 1988, and a St. John’s River Water Management District permit for stormwater facilities in 1991. Lots have been platted, streets have been constructed and homes have been sold. Rosetta Villas Subdivision includes a water retention pond on-site, built in 1995. There is a pipe from that pond which discharges water into a ditch that is partially within the DOT right of way. The ditch has a 30-inch concrete pipe which discharges into DOT’s Pond A. There is some indication in the record that a diversion ditch was part of an over-all permit for the Rose Industrial Park development prior to DOT’s purchase of Pond A. The diversion ditch was intended to convey stormwater around, and not into Pond A. The diversion ditch south of Rosetta Villas and north of Pond A does not convey Rosetta Villas’ run off around Pond A. Instead the 30-inch concrete pipe conveys Rosetta Villas’ overflow water into Pond A. The 30-inch concrete pipe was constructed by BJM in 1995 after an existing, much smaller, pipe became clogged. BJM contends that the pipe was replaced at the direction of someone from DOT. While that contention is not disputed, nothing in this record supports any suggestion that DOT is now estopped from requiring a drainage connection permit. At hearing BJM’s own expert witness opined that the 30-inch pipe which now discharges into Pond A requires a connection permit. (Transcript, p. 130) BJM does not have that permit and, after meetings and extensive discussion with DOT staff, has not applied for the permit.
Recommendation Based on the foregoing, it is hereby, RECOMMENDED: that the Department of Transportation issue its Final Order requiring BJM to apply for a drainage connection permit pursuant to chapter 14-86, Florida Administrative Code. DONE and ORDERED this 24th day of February 1997 in Tallahassee, Leon County, Florida. MARY CLARK Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (904) 488-9675 SUNCOM 278-9675 Fax Filing (904) 921-6847 Filed with the Clerk of the Division of Administrative Hearings this 24th day of February 1997. ENDDNOTE 1/ BJM presented extensive evidence regarding the diversion ditch or swale and its intended purpose. It may be possible for BJM to redirect its out-flow however, the current status of the drainage system. COPIES FURNISHED: Francine M. Ffolkes, Esquire Department of Transportation Burns Building, Mail Station 58 608 Suwannee Street Tallahassee, Florida 32399-0458 Bernard J. Martin, Esquire 506 Wymore Road Winter Park, Florida 32789 Pamela Leslie, General Counsel 562 Haydon Burns Building 605 Suwannee Street Tallahassee, Florida 32399-0450 Ben G. Watts, Secretary Attn.: Diedre Grubbs Haydon Burns Building, MS 58 605 Suwannee Street Tallahassee, Florida 32399-0450
Findings Of Fact On September 13, 1977, SFWMD advised Coquina by letter that "[a]t its September 8, 1977 meeting the Governing Board of this District gave Conceptual Approval of [Coquina's] surface water management plan . . . subject to the four special conditions found on page 15 of the District's staff report. . . [and an] additional special condition Joint exhibit No. 5. The first special condition found on page 15 of the District's staff report requires that complete construction plans be submitted, including "supporting calculations for all design elements not already submitted and any other plans necessary to assure adherence to the concept plan." Joint exhibit No. 2, page 15. The plan approved by SFWMD is designed to lower the water table in a 22 square mile area northwest of Lake Okeechobee in Okeechobee County. In its natural state, the land lies under water for part of the year. The corporate owner of the land has plans to subdivide it and sell residential lots, beginning with the four contiguous sections as to which the present application for a construction permit has been made. These four sections (phase I) lie north and south of each other in the western portion of the larger tract. The proposed construction would consist of digging ditches or swales paralleling existing and planned roads; building intersecting collector swales running north and south; installing ditch checks where swales intersect; dredging a retention pond into which the collector swales could empty at the south end of the phase I tract; digging an outfill ditch to channel water leaving the retention area for Ash Slough; and erecting a weir, between the retention area and the slough. Culverts through the weir would be equipped "with standard flash board risers in which the water level is regulated by stop logs which can be added or removed," Coquina's exhibit No. 1, p. 10, and the culverts would ordinarily serve as the route by which water from the retention area would reach Ash Slough. Under extremely wet conditions, however, water from the retention area could overflow the weir. The intervening petitioners own land on Ash Slough downstream from the retention area and adjacent to the southern boundary of the phase I tract. No formal studies of the likely effects of the proposed construction downstream were undertaken by Coquina or by SFWMD in evaluating Coquina's application. The surface water management plan given conceptual approval by SFWMD provides: The quantity of runoff flowing to the south through existing sloughs will be controlled to protect the downstream areas against flooding whereas at the present there is no control. The amount flowing to the existing sloughs to the south during the 25 yr. design storm will be limited to the amount flowing to those sloughs before any development takes place. Lesser storms will be more completely retained on the property. Controlled discharge will be provided from retention areas to the existing sloughs for the purpose of nourishing these streams. Coquina's exhibit No. 1, p. 1. (Emphasis supplied) Since no records of the amount of discharge to Ash Slough "before any development" are in existence, certain assumptions and estimates were made. One such assumption on which the application for construction permit proceeds is that the phase I tract all drains to the south, in its present state. In fact, some of the water now leaving the phase I tract travels in a westerly direction and never enters Ash Slough, at least under some weather conditions. If the proposed construction is accomplished, the phase I tract would all drain to the south through Ash Slough. As things now stand, a significant amount of water leaves the phase I tract by evapotranspiration. If the water table were lowered two and a half feet, which is what Coquina proposes, less water would leave the phase I tract by evapotranspiration, leaving more water to flow over the ground. In estimating the quantity of the anticipated discharge to Ash Slough, if the proposed construction takes place, it is necessary to take into account drainage onto the phase I tract from adjoining lands. Coquina has failed to furnish plans and supporting calculations sufficient to insure that the proposed construction will not increase the amount of flow to Ash Slough during the 25 year design storm. Increased flow to Ash Slough would aggravate downstream landowners' drainage problems, unless the slough could handle the additional flow, a question which the application does not address. The foregoing findings of fact should be read in conjunction with the statement required by Stuckey's of Eastman, Georgia v. Department of Transportation, 34O So.2d 119 (Fla. 1st DCA 1976), which is attached as an appendix to the recommended order.
Recommendation Upon consideration of the foregoing, it is RECOMMENDED: That SFWMD deny Coquina's application for construction permit. DONE and ENTERED this 14th day of November, 1978, in Tallahassee, Florida. ROBERT T. BENTON, II Hearing Officer Division of Administrative Hearings Room 530, Carlton Building Tallahassee, Florida 32304 (904) 488-9675 APPENDIX Paragraph one of intervening Bass petitioners' proposed findings of fact has been adopted, in substance, insofar as relevant, except that the evidence did not demonstrate that downstream landowners would in fact be harmed. Paragraphs two, three, four, five, six and seven of intervening Bass petitioners' proposed findings of fact have been adopted, in substance, insofar as relevant. Paragraph one of respondent Coquina's proposed findings of fact has been adopted, in substance, insofar as relevant, except for the date of the application. Paragraphs two, three, four, five, six, seven, eight, nine and thirteen of respondent Coquina's proposed findings of fact have been adopted in substance, insofar as relevant. Paragraph ten of respondent Coquina's proposed findings of fact stated a conclusion of law, in part. While "testimony was presented that the construction of Phase I would have no substantial adverse affect [sic] on surrounding properties," the evidence as a whole did not establish this fact. Paragraphs eleven and twelve of respondent Coquina's proposed findings of fact have not been adopted because they were not established by the evidence, except for subparagraph eleven (f), which was proven. COPIES FURNISHED: John Henry Wheeler, Esquire South Florida Water Management District Post Office Box V West Palm Beach, Florida 33402 Robert Birenbaum, President Viking Communities Corporation (Coquina Water Management District) 123 Northeast 70 Street Miami, Florida 33138 Kyle S. Van Landingham, Esquire County Attorney Okeechobee County Courthouse Okeechobee, Florida 33472 Andrew B. Jackson, Esquire J.C. Bass & Bass Ranch, Inc. Post Office Box 488 Lake Placid, Florida 33852 Emerson Allsworth, Esquire 1177 Southeast Third Avenue Ft. Lauderdale, Florida 33316 Mr. Bob Wittenberg Division of Florida Land Sales and Condominiums The Johns Building 725 South Bronough Street Tallahassee, Florida 32304 Dr. Patrick M. McCaffrey Kissimmee Coordinating Council 2600 Blair Stone Road Tallahassee, Florida 32301 Mr. George Stansbury Central Florida Regional Planning Council Post Office Box 2089 Bartow, Florida 33830
Findings Of Fact The Parties The Applicant, Trail Ridge Landfill, Inc. (Trail Ridge), is a corporation formed in 1989 for the purpose of developing a landfill project and providing waste disposal capacity for the City of Jacksonville. Trail Ridge Landfill, Inc. is a wholly-owned subsidiary of Waste Management of North America, Inc. Its operating division is involved in the waste collection, recycling and disposal business. Waste Management of North America, Inc. is a wholly-owned subsidiary of Waste Management, Inc., which is involved in all facets of solid waste collection and disposal nationally. The Florida Department of Environmental Regulation (DER) is an agency of the State of Florida charged with the responsibility of regulating solid waste management facilities and with permitting their initial construction and operation. It is charged with reviewing applications for permits for construction of such facilities, for reviewing applications for dredge and fill permits in wetlands or waters of the State and, as pertinent to the project involved in this proceeding, for storm water management and storage of surface water and the regulation thereof through its permitting and enforcement authority contained in Chapters 403 and 373, Florida Statutes, and Titles 40C and 17, Florida Administrative Code. The Petitioners are Coastal Environmental Society, Inc. (CESI), a not- for-profit Florida corporation established for the purpose of protecting natural resources. St. Johns Preservation Association, Inc. (SJPA), also a not-for- profit Florida corporation established for the purpose of protecting the community, including environmental concerns; Baldwin-Maxville Coalition, Inc., also a not-for-profit corporation established to promote the health and welfare of its community, including environmental concerns; William McCranie, a resident of Jacksonville, Florida; Darryl Sperry, a resident and citizen who lives 1 1/4 miles from the proposed landfill site in Baker County. All Petitioners have been established to be substantially affected by the proposed permitting and the projects related thereto and all have met pertinent standing requirements as a matter of fact and law. The Respondents do not contest the standing of the Petitioners. Background and Purpose of the Project The purpose of the proposed landfill facility is to address the solid waste disposal needs of the City of Jacksonville and Duval County (the City). The City currently disposes of solid waste at two landfills. One is on the east side of Jacksonville on Gervin Road, and the other is located in the north area of Jacksonville on Island Road. The presently used, east landfill is an unlined landfill currently operated pursuant to a DER Consent Order, in connection with which closure of that landfill is planned. The north landfill consists of three unlined cells and one lined cell. The City currently has unused landfill capacity at these two landfills which will last approximately one more year, but has also sought approval for expansion of the north landfill which would provide about two more additional years of capacity, if approved. The proposed landfill project, if approved, constructed and operated, would meet these solid waste disposal needs for approximately 20 to 25 years. The project at hand began when the City issued a Request For Proposal for private companies to submit bids to the City for construction of additional landfill capacity somewhere to the northwest of Jacksonville in Duval County. Two companies that met qualifying requirements submitted proposals in response to the request for proposals. Trail Ridge was one of those two qualifying bidders. The City selected the Applicant for contract award and then entered into a contract. The Applicant has an option to purchase the proposed landfill site from Gilman Timber and Land Company (Gilman, Gilman Paper Company). After issuance of the permits to the Applicant, the option would be exercised. Thereafter the property would be immediately conveyed to the City from the Applicant. Thus the site of the proposed facility will ultimately be owned and controlled by the City, although the Applicant will operate the landfill under its contract with the City. Gilman presently uses the 1,288 acre site and several thousand surrounding acres for growing timber, principally pine trees, in a pine plantation-type operation grown for use as pulp wood. Much of the site and surrounding Gilman land is characterized by pine trees grown to an age of 20 years or less and then harvested. A great deal of the site property has recently been cut, chopped, plowed re-bedded and re-planted with pine trees. Although some of the site is characterized by mature timber, much of the timber has been recently planted or is otherwise timber not yet mature enough for harvest. The option agreement provides that Trail Ridge will purchase the property from Gilman for $10,000 per acre. The City will then purchase the 1,288 acres from the Applicant for $2,600 per acre, which the Applicant maintains is the current, fair-market-value for the land as it is currently used as pine plantation for growing pulp wood. These terms and conditions are a part of the City's Request For Proposals. In addition to paying the Applicant $2,600 per acre for the 1,288 acre site, the City will pay the Applicant a fee over the life of the operation of the proposed landfill. The fee, amortized over the 20- year span of the agreement, will make up the difference between the Applicant's $10,000 per acre purchase price paid to Gilman and the City's $2,600 per acre initial purchase price paid to the Applicant. The City will thus ultimately re- pay Trail Ridge the $10,000 per acre for the purchase price for the property. The Applicant corporation will operate the landfill over its entire useful life and then close it. Thus, the Applicant's own figures show the land is valued at $3,348,800. The record does not reflect the reason for the purchase price paid to Gilman being $12,880,000, of which the City will repay $9,000,000 to the Applicant in the form of the operation fee, over and above the initial payment to the Applicant of $3,348,800. In any event, the utilities payment to the Applicant of the $12,880,000 for the land and the operation of the landfill only represents the recompense to the Applicant for the purchase funds expended for it to buy the site from Gilman. Additionally, the Applicant, through its option agreement with Gilman, is required to pay Gilman a $60,000 per month option fee. $15,000 per month of that must be paid during the pendency of the option, with the remainder of the $45,000 monthly fees due upon closing of the purchase. The portion of the operation fee paid by the City over and above the $2,600 per acre initial purchase price, attributable to the land appraisal itself, will be paid by the City on the basis of a certain dollar fee-per-ton of solid waste handled and disposed of in the landfill by the Applicant. Testimony indicates this will be approximately $8.00-$15.09 per ton, although the evidence as to which amount is indefinite. The testimony of Applicant's witness Allen, in any event, references these amounts as applicable to the City's solid waste "stream" handled by Trail Ridge at the proposed facility. Its contact with the City assures the Applicant of a minimum of 569,000 tons of waste per year to which the fee would apply. The City currently generates approximately 750,000 tons of waste per year. There is no evidence of what the construction or other capital costs or operation expenses related to the proposed facility will be over the useful life of the facility for the Applicant or related corporations. Site and Design The proposed site is 1,288 acres in size, located in southwestern Duval County, approximately three miles south of Interstate Highway 10, 1.5 miles west of U.S. Highway 301 and 1.14 miles north of State Road 228. The site is located in a sparsely populated area approximately 4 to 6 miles from the City of Baldwin, 5 miles from the City of Macclenny and 2 miles from the City of Maxville. A substantial portion of the proposed site will be left undisturbed and used as a buffer area to separate it from any surrounding development. There are water supply wells within fairly close proximity to the site. One well is within a mile of the site and three are approximately 1.5 miles southeast of the site. The proposed facility will include both a Class I and Class III solid waste disposal area. The Class I area will be approximately 148 acres in size, and the Class III area, 28 acres. The Class III disposal area will only be used for non- household refuse such as construction debris, tree and shrubbery clippings and the like, which will not generate deleterious substances in liquid or gaseous form, as will the Class I landfill. The remainder of the 1,288 acres will be used for buffer zones, dirt borrow areas, storm water management facilities and ancillary facilities necessary to the day to day operation of the landfill. No part of the Class III disposal area will be located within 200 feet of jurisdictional wetlands, which are the closest bodies of water. The project will be located on "Trail Ridge," which is a relatively elevated geographic feature, extending generally in a north-south direction in western Duval County. Geologically, it is an ancient sand dune. There is a substantial decline in elevation of this portion of the ridge from west to east, which produces surface water drainage patterns in a west to east direction at the site, also accompanied by surface water drainage patterns in a southerly- northerly direction into wetlands which occur on the south and north verge of the site, because the site is a prong or easterly extension of Trail Ridge lying between wetlands which occur on the northerly, southerly and easterly boundaries of the Class I disposal site. The 1,288 acres, including the landfill sites themselves, have been used for silvi-culture practices since 1948 or earlier, and are currently managed primarily as a slash pine plantation grown for pulp wood purposes. The present owner of the site, Gilman Paper Company, plans to continue this use of the site should the landfill project not be approved and constructed. Since 1948, the entire site, including much of the wetlands thereon, have been logged, some portions of it as many as three times. The silvi-culture practices at the site include clear- cutting, chopping, burning, harrowing, tilling and bedding of the soil, and planting of pine trees. The pine trees are grown to be harvested on a 20-year cycle or less. Due to these intensive silvi-cultural practices, the natural conditions of the site have been significantly altered and much natural vegetation, such as bottom-land hardwoods, has been replaced by planted pine trees. The area has been extensively ditched for drainage purposes and logging roads have been constructed throughout the site. The design of the Class I disposal area of the landfill includes three major components: a liner system, which includes a permanent leachate collection and removal system, a cap and closure system and a gas control system. The Class I disposal area is designed to be 140 feet high when the landfill is completed and closed in approximately 20-25 years. It will have typical landfill refuse "lifts," of approximately 8 to 12 feet in height, with a side slope grade of three horizontal feet to one vertical foot of elevation gain. This is the maximum grade steepness allowed by DER rules. The Class III landfill, in which no household garbage, chemicals, oils and greases or other deleterious substances will be deposited, will include only a cap and closure system. In order to carry out Department regulatory requirements designed to contain waste permanently in a well- defined area and to minimize the amount of leachate produced within a landfill, as well as to collect and remove leachate that is produced, the landfill will have, in effect, a double liner system. The liner system is designed to contain the leachate produced when rain water contacts waste in the landfill and to cause that leachate to percolate vertically downward through the landfill, capture it in the liner system, prevent it from contacting groundwater and to remove it and treat it. Leachate from the Class I disposal area will be contained by the liner system and removed by a leachate collection and removal system. The liner system, starting from the bottom and proceeding upward, will consist of a 6 inch thick layer of compacted, subgrade soil. Over that layer, a prefabricated "bentonite" clay-like material will be deposited. Directly over the bentonite layer will be a high density polyethylene liner (the secondary liner) called a "geomembrane." The bentonite material has the characteristic of swelling when contacted by a liquid so that, if the geomembrane leaks, the bentonite will swell and plug the hole in the liner above it. On top of the bentonite layer and the geomembrane layer, is a synthetic drainage material called "geonet." Geonet has a very high transmissivity rate and therefore has great capacity to conduct water within its own plane. Lying immediately above the geonet material is a geotextile filter designed to keep sand out of the pores or interstices of the geonet. Above that geotextile filter is a second geomembrane (the primary liner). Above the second geomembrane is another geonet layer, as well as another geotextile filter layer. Then to protect the entire liner system from damage, two feet of clean sand will be placed above the uppermost geotextile filter layer. The two feet of sand also acts as a drainage layer for the uppermost geonet. The leachate that percolates down through the waste and the sand will contact the geonet and then be carried down slope on top of the geomembrane. This constitutes the leachate collection system. The bottom geonet is called the "leak detection system." This is because, if a hole develops in the primary liner, any leachate coming through the hole will be quickly drained away through the bottom geonet. The bottom geonet thus operates as a backup leachate collection system, since any leachate reaching the bottom geonet will also be discharged into the leachate removal system. If a leak should develop in the secondary liner, the bentonite material would quickly plug the leak, swelling and absorbing that liquid. The Petitioners have stipulated that the Applicant has proposed a liner system and leachate collection system for the Class I disposal area which meets all criteria of Chapter 17-701, Florida Administrative Code, except as to the requirements of Rule 17-701.050(5)(c), (e)3. and 4. and (f)3., Florida Administrative Code. The Applicant demonstrated that the liner system and leachate collection system will meet the criteria of Rule 17- 701.050(5)(c), Florida Administrative Code. The liner system will be installed in accordance with a quality assurance plan. A specific condition already agreed upon will require the Applicant to submit for approval a revised quality control and assurance plan for installing the Class I synthetic liner system, after selection of the liner manufacturer and prior to the liner's installation. The liner system is designed so that it will be protected from puncture by waste materials or landfill operation equipment. In addition to the two feet of sand placed on top of the entire liner system to protect it, when initial waste disposal begins, the first lift of waste across the entire area of the liner system, as it is installed in phases, will be composed of 6-8 feet of "select waste" to protect the liner from puncture. Select waste is waste containing no pipes, roots or other potentially puncturing objects which could penetrate the sand layer to damage the liner system. A quality assurance engineer will be on site full-time supervising the initial placement of the select waste until that phase of the landfill operation is completed. A grant of the permit should be so conditioned. The Applicant has established that the liner system and leachate collection system will meet the criteria of Rule 17-701.050(5)(e), Florida Administrative Code. The leachate depth on top of the primary and secondary liners will not exceed a foot because the geonet has the capacity to quickly remove leachate from the liner. The actual hydraulic head of leachate on the primary liner will be only approximately 1/4 inch. The depth on the secondary liner was shown to be even less. The liner system and leachate collection system will meet the criteria of Rule 17-701.050(5)(e)3. and (f)3., Florida Administrative Code. The design of the collection system, including the geotextile filter, will prevent clogging of the system throughout the active life and closure period of the landfill, primarily by placing a gravel aggregate around the collection pipe so as to prevent debris from entering the system. A pilot line will also be installed in each collection pipe to facilitate access for mechanical cleaning, should it be necessary. In the unlikely event of an obstruction in the system, the leachate would simply bypass that area and continue down-grade to the next downstream leachate collection pipe and be removed from the landfill for treatment by that means. The liner system and leachate collection system will also meet the criteria of Rule 17-701.050(5)(e)4., Florida Administrative Code. The leachate collected will be carried downhill to pipes at the east end of the landfill. The leachate will then be pumped from the pipes into storage tanks. Trucks will then be filled with leachate to be transported to the City's Buckman Regional Wastewater Treatment Plant, owned and operated by the City, for treatment and disposal. Unrefuted evidence shows that this plant has adequate capacity and treatment capability to safely treat and handle the leachate. The truck loading areas will be equipped with berms and other means of protecting the surrounding wetlands, surface and groundwaters from leachate spills during the truck filling process. The Applicant's evidence does not demonstrate, however, that the tanks themselves and the area surrounding them will have protective measures for containing leachate spills. In order to comply with the above rule, the totality of the evidence concerning the leachate collection, disposal system and treatment method demonstrates that the tanks should be accompanied by a surrounding containment system (walls or berms) which will have the capability of containing the entire capacity of a tank should failure of a leachate collection tank or related piping or valving occur. Any grant of the permit should be so conditioned. The Petitioners have stipulated, and the Department agrees, that the Class III disposal area is exempt from the liner system and leachate collection system requirements of the above-cited rule provisions. Covering and Closure System Both the Class I and Class III landfills are designed with a composite soil covering system to minimize the amount of rainfall which can come into contact with the solid waste so as to minimize the creation of leachate. During the day to day landfill operations, a 6 inch initial cover will be applied to enclose each Class I landfill disposal cell on a daily basis, except for the working face itself, where waste is currently being deposited. The working face may be left uncovered, so long as solid waste is scheduled to be placed on it within an 18 hour period. A 6 inch initial cover will also be applied once every week to enclose each Class III landfill disposal cell. Thereafter, an intermediate cover of one foot of compacted earth will be applied on top of the initial cover within seven days of initial completion, if a final cover or additional lift on top of that completed cell is not to be applied within 180 days of cell completion. The initial cover will consist of sandy soil, over which will come the intermediate cover of one foot of compacted earth. The final cover will be applied to those portions of the landfill which have been filled with waste to the extent of designed dimensions at the time those portions have been filled. The final cover, to be placed on the sides of the landfill and ultimately upon the top at the end of its useful life, will be placed on top of the 12 inches of intermediate soil layer and will consist of 12 inches of compacted clay with a permeability of 1 X 10/-7 cm/sec. Next will come a layer of 12 inches of compacted soil and then a final layer of 12 inches of top soil, upon which the Applicant will plant grass for erosion control. Erosion of the cover layers on the side slopes is designed to be minimized by closing areas of the landfill as they are filled, an operational procedure commonly referred to as "close as you go." The final cover layers placed on the landfill outside of the clay cap are designed to allow the establishment of a planted grass cover as soon as possible to minimize erosion of the cover material and the side slopes. In addition, the intermediate cover placed on top of and between each cell, beneath the clay layer surrounding the outside perimeter of the landfill, has a high permeability, thereby acting as a drainage layer to direct rainfall and leachate vertically downward to the leachate collection system, as well as to collect runoff so as to retard erosion. Erosion is also retarded, as is the runoff of storm water/leachate over the side slopes of the landfill, by containing storm water which comes into contact with the working face of the landfill cells. This will be accomplished by minimizing the size of the working face to approximately 42 feet width. This will serve to reduce the potential for storm water to contact waste. Additionally, berms will be constructed around the working faces of each active cell which will cause any runoff or storm water which gets inside the working face of the cell to remain there and to percolate through the land fill to eventually be collected as leachate by the collection system. If enough rain falls on the working face of a cell to cause an overflow of storm water over the berms, additional berms placed on the interior slopes of the landfill will catch the overflow and divert it back through the landfill and the leachate collection system. The Applicant contends that normal maintenance equipment and personnel will be able to maintain the exterior side slopes of the landfill and thus minimize erosion. However, if erosion should become a problem, the Applicant proposes to install interceptor berms constructed on the side slopes, accompanied by various geotextural fabrics or synthetic materials proposed to be imbedded on the side slopes to help anchor the interceptor berms. These berms, however, have been demonstrated by Petitioner's witness, Mr. Peavy, to be inadequate to retard erosion. In fact, they may promote erosion because they would be insufficiently anchored to the side slope (as designed with 3:1 slope) and the downhill slope of the berms themselves is considerably steeper than a 3:1 ratio, which will actually promote erosion. The erosion problem will be discussed in further detail infra, but the proposed "optional" berm system, consisting of two proposed berms down the length of the 450 foot side slope will have to be redesigned in order to serve the purpose of retarding side slope erosion. The cap or cover for the exterior side slopes of the landfill will consist of a relatively impermeable clay layer overlain by a sand layer, as well as a top soil layer. Mr. Lithman, an expert in geotechnical engineering testifying for the Applicant, established that as a result of the side slope stability analysis he conducted of the clay layer for the Class I disposal area, that the clay layer would be stable, with a safety factor of 2.9-3, which is more than adequate for a slope as designed for the Class I disposal area (3:1). Mr. Evander Peavy, testifying for the Petitioners and accepted as an expert witness in the fields of civil engineering, soil mechanics, surface water hydrology and hydraulics, agreed that there was an adequate safety factor in the clay cap layer itself and that no plane of failure would likely occur in that layer. The problem, however, lies in the sand layer immediately predetermined or potential plane of failure will occur at the interface between the sand layer and clay layer. This is where the side slope of the landfill is most likely to fail. Failure means that the weight of the sand and soil layers on the outside of the clay layer would exceed the resisting forces, holding them back on the slope of the landfill, which would result in a deformation, slumping or break in the sand layer. If this slumping or break occurs in the sand layer and is not immediately repaired, rain water can erode the clay layer, which is highly erodible if exposed to rainfall. If not redressed soon, this could result in exposure of the waste of the landfill to rain water with the result that leachate could seep out of the side slopes of the landfill and enter surface waters of the State through the functioning of the storm water system. The most likely layers a civil engineer would analyze to determine the stability of the side slope would be the sand and soil layers above the clay layer because they are the weaker layers in terms of adhesion, shearing and resistance to downward movement under stress. However, Mr. Lithman, Trail Ridge's expert who conducted a side-slope stability analysis, only analyzed failure in the clay layer initially, until he was called on rebuttal to address findings of Mr. Peavy. The DER rule provision that allows 3:1 ratio side slopes for the sides of such landfills only serves as a guideline or maximum steepness criteria for design engineers. It does not relieve an engineer from analyzing slope stability in accord with good engineering practices. Analyzing side slope stability must be done in terms of establishing "safety factors." An acceptable safety factor for a landfill is 1.5 because, if failure occurs, solid waste can quickly be uncovered which can cause leachate contamination to surface waters of the State. A safety factor of 1.5 is the commonly accepted factor for earthen dam design because of the risks posed by failure of such slopes or embankments. Mr. Peavy is extensively experienced in the design of earthen dams and similar earth works, including extensive analysis of slope constituents and design for stability under shear forces and other failure-inducing factors, as well as for resistance to erosive forces. He was engaged in such phases of engineering work for approximately 26 years, during which period he designed and oversaw construction of numerous dams, revetments and other earthen embankments and works of many types. Because of this, and because of the commonly accepted engineering methods and calculations he used in analyzing the stability and integrity of the side slopes of the landfill, involving plane of failure analysis and erosion damage analysis, his testimony is credited over that of the other witnesses testifying on the subject matters involving side slope integrity of the landfill. Because of this, a safety factor was established for the side slopes of the landfill, for the sand and soil layers of 1.5. Safety factors of 1.25 are indeed commonly used for highway embankments, but highway embankments are not designed with predetermined or potential planes of failure, such as is involved at this landfill (as presently designed) between the sand-soil layers and the clay layer. Trail Ridge's expert witness in this area, Mr. Lithman, had testified that a safety factor of 1.25 would be adequate because it was typical of DOT earthen embankments for roadways. Mr. Niehoff testified that a 1.3 safety factor was sufficient. In fact, however, Mr. Peavy, testifying for the Petitioners, calculated the safety factor of the side slopes of the landfill to actually be 0.85, using his initial assumption of a weight for a cubic foot of the sand-soil layer of approximately 100 pounds. Mr. Niehoff testifying for Trail Ridge found no basic fault with Mr. Peavy's analysis of the safety factor and alleged that his analysis was done with accepted engineering procedures, but only with use of slightly different assumptions. He testified that if he had used the same assumptions as Mr. Peavy, he would have reached the same conclusions. Mr. Peavy also calculated his safety factor again by employing the same equation used by Trail Ridge's expert, Mr. Lithman, and assumed instead that the unit of sand-soil layers was 125 pounds per cubic foot, as did Mr. Lithman. This assumption coupled with the internal angle of friction of 35 degrees used by Mr. Peavy, which was shown to be a conservative assumption, resulted in a calculated safety factor of 1.05, which is still unacceptable, even under Mr. Lithman's analysis, because Mr. Lithman opined that the safety factor should be 1.25. Using Mr. Peavy's equation, but his own assumptions as to angle of friction and weight per cubic foot of the sand-soil layer, Mr. Niehoff, testifying for the Applicant, calculated a safety factor of 1.3. This safety factor also is unacceptable because it is less than the 1.5 safety factor established as proper by Mr. Peavy's testimony and, indeed, if Mr. Lithman's safety factor of 1.25 could be deemed acceptable, the 1.3 figure would result only in a marginal safety factor at best. The major difference between the safety factor calculations of Mr. Peavy and Mr. Niehoff is that Mr. Peavy assumed that the sand-soil layer above the clay layer would be saturated, while Mr. Niehoff assumed that only 19 inches of the 24 inch sand-soil cover layer would be saturated by rainfall. However, Trail Ridge's own experts, Mr. Lithman and Mr. Niehoff, offered conflicting testimony between themselves on the amount of saturation to be expected. Like Mr. Peavy, Mr. Lithman did his analysis on the basis that the sand-soil layers would be saturated completely, contrary to Mr. Niehoff's subsequent testimony that this would not happen beyond a 19 inch depth in the layer. Mr. Niehoff's conclusions that the sand-soil layer would not become saturated or valid only if there is a complete grass cover over the entire side slopes of the landfill. He admitted that if the sand-soil layer became saturated, the safety factor would only be 1.1 or less according to his own calculations. Trail Ridge offered no preponderant evidence to establish that an adequate grass cover could be established so as to prevent saturation of the sand-soil layer during the design 25-year, 24-hour storm event (approximately 8- 9 inches rainfall in 24 hours). The evidence indicates, rather, that establishing and maintaining a grass cover on the side slopes of the landfill will be very difficult to achieve on a uniform, completely grassed basis. This is because of erosion and because of the damage by equipment necessary to repeatedly repair erosion damage and because of the fact that much of the side slopes of the landfill will be, in effect, under construction until the landfill is completely built out and completed at the end of approximately 20 years. Even if the lower several lifts of the landfill, when covered on the "cover as you go" basis can achieve them, more recently deposited, will not have a complete grass cover. Thus, there is a substantial likelihood of saturation of the sand-soil layer, during storm events of the type for which the landfill is designed. Further, the volume of water that would saturate into the sand-soil layer, even if the landfill was completely grassed, will still be sufficient to totally saturate the lower 90 feet of the landfill side slopes above the clay layer in the event of a 25-year, 24-hour storm event. If the sand-soil layers become saturated, sloughing or failure of those layers will occur at the toe of the landfill. If that occurs, then the clay layer, protective cap can be quickly eroded by subsequent rainfall and surface runoff. This will cause the waste within the landfill to be exposed to rainfall, generating leachate which can migrate to the surface of the landfill and thence to the storm water system and ultimately to the surface waters of the State. No provisions have been made in the design to remove water from the sand-soil layers once it reaches the area near the toe of the landfill to prevent sand-soil layer failure. The impermeability of the clay layer would prevent the rainfall from migrating through the clay layer and continuing to the interior bottom of the landfill to be collected properly as leachate because the clay layer properly should be an impermeable barrier to storm water. Thus, a saturated condition of the sand-soil layers would be most likely to cause their sloughing and failure near the toe of the landfill, with resulting damage by erosion or cracking to the clay layer with the effect of allowing leachate to escape to surface waters of the State. Although the Applicant's expert, Mr. Lithman, opined that side slope stability had not been a problem with the 3:1 ratio slopes at the City's Rosemary Hill Landfill, he admittedly was unaware of the height or length of the side slopes of that landfill. The longer the side slopes and the higher the landfill, the more likely it is that the sand-soil layers will become saturated and fail during design storm events or shortly thereafter, especially as the landfill, in its later years is built both longer and higher toward its final configuration. Further, Mr. Lithman and the Applicant's evidence does not reveal the composition of the side slopes of the Rosemary Hill Landfill, in terms of whether or not the clay and sand-soil layers designed in the proposed landfill are present. Due to the height of the proposed landfill, the lengths of its side slopes and the absence of design features such as terraces and benches, failure of the side slopes, especially in the later years of the landfill's life and, indeed, after closure (closed landfills can generate leachate) is likely to occur, based upon the facts established through Mr. Peavy's testimony. The likely side slope failure is a result of the design flaw and is not a problem which can be cured by normal operation and maintenance activities. Indeed those activities may aggravate the problem through their deleterious effect on the establishment of a uniform, complete grass cover. Because of the height of the proposed landfill, the length and slopes of its sides and the lack of design features such as benches or terraces, it is likely to experience significant side slope erosion due to storm water. The volume of rain water that would accumulate and flow down the sides of the landfill will achieve velocities which would destroy even a well established grass cover, especially in the later years of the landfill's life when the sides have reached significant length and height. Storm water would thus gain sufficient velocity to destroy a grass cover and to particularly attack those portions where the grass cover is incomplete, thinned or possessed of an insufficient root mat to hold the soil. Once erosion starts, small rills will form which will soon develop into deeper gullies, ultimately penetrating the sand-soil layer. It can then quickly erode away the resulting exposed clay cap layer, exposing the waste to storm water. Leachate could thus leak from the landfill. Because of the present design of the Class I landfill, the only way to repair erosion damage is to push material from the bottom with heavy machinery, such as bulldozers. These erosion maintenance activities themselves would prevent the establishment of a uniform solid grass cover. The presently operated East Landfill in Duval County exhibits both side slope failure and erosion damage due to rainfall on its 3:1 slopes, including damage to the grass cover. Erosion damage to the slope layers due to erosion maintenance activities of the type which would be necessary to repair damage at the proposed landfill has occurred. Both erosion and side slope failure will ultimately result in exposure of solid waste to rainfall runoff and assure side slope seepage of leachate. The material eroded or sloughed away from the side slopes can obstruct the drainage conveyance system surrounding the landfill, rendering the MSSW/storm water system inoperative. Because of the presently proposed design of the landfill, it would be impossible to effectively correct side slope erosion or failure, due especially to maintenance activities. Even if a uniform grass cover could be established in the last years of landfill operation and after closure, the great length and slope of sides of the landfill by that time would result in erosion even if the grass cover were initially uniform and solid on the entire slope of the landfill. A change in the design of the landfill, however, whereby 15 foot wide benches or terraces would be incorporated into the sides of the landfill every 20 or so vertical feet, would likely prevent the side slope erosion and failure established to be likely by Mr. Peavy. In fact, benches or terraces similar to those found to be required by Mr. Peavy have had to be recently installed at the East Landfill in Duval County in order to resolve side slope erosion and failure problems on those 3:1 slopes. The mere installation of interceptor berms, as depicted in TRL Exhibit 28, would not alleviate side slope failure and erosion problems, but rather would aggravate them and would reduce the safety factor of the side slopes to 0.5. Consequently, in order to grant the permit, it should be conditioned on the landfill being re-designed and constructed so as to incorporate benches or terraces at approximately 20 foot intervals on the slope of the landfill from bottom to top. Although this may potentially reduce the volume of space within the landfill, depending on how it is accomplished, it has been established that, without the use of the bench or terrace system, pollutant leachate cannot be reasonably assured to be prevented from entering State waters and wetlands. Leachate Control Leachate is any water coming in contact with solid waste. The chemical constituents of leachate which are present and will be present in the Duval County solid waste stream, to be disposed of at the proposed landfill, include chlorobenzene, volatile organics of various types, benzene, acetone, phenolic compounds, gasoline constituents, chloroform, methylethylketone, methylene chloride, toluene, xylene, ethylbenzene, total organic carbon, nitrogen, phosphorus and metals such as aluminum, chromium and zinc. Leachate thus contains toxic, hazardous and priority pollutants which will be disposed of in the landfill. The breakdown and degradation of solid waste can also generate additional toxic or hazardous compounds and substances. Leachate can potentially be discharged in a proposed landfill into groundwater and surface waters in a number of ways, including leakage from the bottom of the landfill liner into groundwaters, including into the Class I storm water pond and surface waters of the State through discharge from the groundwater into the storm water pond system. It could also be deposited into the storm water system through spillage of leachate where tanker trucks are loaded, through seepage of leachate through the side slopes of the proposed landfill by damage to the integrity of those side slopes as found above. The Petitioners maintain that side slope seepage of leachate will occur because the permeability of the intermediate cover layers surrounding the cells of the landfill is significantly less than the permeability of solid waste. This will have the result, according to Petitioners, that leachate will migrate horizontally through the intermediate cover layers to the sides of the landfill. Once there it arguably would migrate to the surface of the landfill side slopes through erosion of the outer cover, and fissures in the clay due to drying from exposure to the sun and through erosion. Additionally, the Petitioners maintain that leachate will migrate downward through the peripheral intermediate cover layer under the clay and contact the impermeable clay anchor cap, build up hydraulic head pressure and thus seep out through landfill sides near the toe of the landfill. The Petitioners maintain that Trail Ridge's policy and proposal to punch holes in the intermediate cover layers atop the cells of the landfill to encourage downward migration of leachate and discourage horizontal migration of leachate through the intermediate cover layers will be ineffective because the intermediate cover is more permeable than the solid waste itself so that punching holes in the intermediate cover to allow the leachate to migrate down through solid waste will actually not occur. Additionally the Petitioners contend that the filter system and the storm water pond will not treat the dissolved chemical components of the leachate specified in Petitioner's Exhibit 2 and that these dissolved components will move through the sand filters into waters of the State. Contrary to Petitioner's contentions, however, the Applicant has demonstrated that leachate will not avoid capture by the leachate collection system by seeping horizontally through the cover or cap and out the sides of the landfill, provided that the side slope failure and erosion prevention measures found to be necessary in the above Findings of Fact are instituted in the design, construction and operation of the landfill. The design of the cap and closure system is basically a side slope seepage prevention system, except for the absence of terraces or benches. The intermediate soil cover beneath the clay cap and surrounding each cell of the landfill acts as a drainage medium. It will channel any seepage of leachate from the cells of solid waste through the permeable, intermediate soil cover, generally in a downward direction, both in and between the cells of the landfill throughout its cross-section, as well as downward through the intermediate soil cover lining immediately beneath the clay cap around the periphery of the landfill. This system, if the above design deficiency is corrected, will tend to force the leachate downward into the collection system, as opposed to horizontally out the cover or the sides of the landfill. The reason this system will work in this manner is because the intermediate cover soil is more permeable than the solid waste itself. The permeability of the intermediate cover will promote vertical movement of the leachate because, as the leachate migrates across each cell, it will encounter the vertical, intermediate soil cover layer at the side of each cell and that will promote its moving downward toward the collection system. The water in the landfill will thus follow the path of least resistance, so that the vertical portions of the intermediate cover layers surrounding each cell and surrounding the sides of the landfill beneath the clay cap, coupled with the force of gravity, will provide a preferential path downward toward the leachate collection system. This finding includes consideration of the Petitioners' contention that leachate will migrate downward and contact the impermeable clay anchor cap and build up head pressure so that it will seep out of the sides at the toe of the landfill. The intermediate cover layer underlying the sides of the landfill beneath the clay anchor cap is connected with the leachate collection system underlying the bottom of the landfill. Thus, a continuous conduction of leachate down through the intermediate cover, permeable layer will allow the leachate to seep downward all the way to the leachate collection system rather than pooling behind the impermeable clay anchor cap. This condition will be enhanced by the fact that surrounding each cell is the approximately vertical, permeable intermediate cover layer, throughout the entire cross-section of the landfill, such that much of the leachate will migrate downward in the interior of the landfill. Because of the ready conductance of leachate in a downward direction by the intermediate cover layers, Trail Ridge's policy of punching holes in the intermediate cover layer on the top of each cell in order to seek to prevent side slope seepage of leachate will be ineffective because the intermediate cover is more permeable than the solid waste. Thus, this procedure is unnecessary and, in fact, could become counter-productive to the extent that punching holes in the intermediate cover would allow rain water mixed with leachate to contact more of the solid waste contents of the landfill as it migrates down through the interior of each solid waste cell. This would result in a more highly concentrated form of leachate, which could pose more deleterious threats to ground and surface waters should it escape to ground and surface waters. Therefore, any grant of the permit should be conditioned on a prohibition of the Applicant thus violating the integrity of the intermediate cover layer overlying each cell as the landfill is built up in lifts. Gas Control System The Class I disposal area is designed with a gas control system which will prevent explosions and fires caused by the accumulation of methane gas due to decomposition of the waste in the landfill. The gas control system will prevent damage to the vegetation on the final cover of the closed portions of the landfill or vegetation beyond the perimeter of the property. It will prevent objectionable odors off site. The Petitioners have stipulated that the Applicants' gas control system will be designed in accordance with Rule 17- 701.050(5)(j), Florida Administrative Code. Although the Petitioners presented testimony of various persons who live in close proximity to other landfills, which were at one time operated by Waste Management subsidiary companies, neither the persons who testified of odor problems at those landfills, nor other witnesses presented testimony to show whether any of the landfills utilized a gas control system or one of equivalent design to that proposed for the subject facility. No evidence was presented to support a finding that the proposed landfill facility would produce objectionable odors to any significant degree. The Petitioners have further stipulated that the Class III disposal area is exempt from the gas control system requirements set forth in Rule 17- 701.050(5)(i) and (j) and (6)(i), Florida Administrative Code, and the Department agrees. Hydrogeology and Ground Water Monitoring The Applicant filed as part of its application, and placed in evidence, a hydrogeological survey and groundwater monitoring plan, contained in TRL Exhibit 51. The hydrology of the proposed landfill site may fairly be characterized as complex because it contains many different features such as recharge and discharge areas, varying zones of conductivity, a sand component to the surficial aquifer as well as a rock aquifer component and multi-directional groundwater flows. Additionally, wetland systems occur down-gradient from the higher levels of the surficial aquifer on the north, east and south sides of the proposed Class I disposal area. From the surface grade down to a depth of approximately 100 feet lies the surficial aquifer, which primarily consists of a coarse sand medium. Lying below the sand aquifer is a confining unit (relatively impermeable) identified as the Hawthorn Group, which consists of denser marls, dolomites and silver clays. Beneath the Hawthorn layer, at a depth of approximately 300-400 feet, is the Floridan aquifer, which serves as the principal deep water supply source for this part of Florida. Additionally, immediately above the Hawthorn layer in the deep zone of the surficial aquifer, a "rock aquifer" exists under a portion of the landfill site, generally the eastern-most portion. It was not shown to be continuous throughout the site. The rock aquifer is connected to the sand surficial aquifer lying above it. Zones of varying higher and lower permeability occur at various places within the surficial aquifer. Generally, groundwater at the site flows down-gradient in an easterly direction, caused by rain or surface water recharging the surficial aquifer on the higher portions of Trail Ridge, including the western side of the landfill Class I disposal site. The surficial aquifer then discharges this groundwater to the land surface and the wetlands lying on the eastern side of the site. Additionally, some northward and southward flow of groundwater occurs from recharge areas to the wetlands lying on the northerly and southerly boundaries of the Class I disposal site in the wetlands. The specific condition 19 contained in the Department's Notice of Intent to issue permit and draft permit requires the Applicant to periodically (quarterly) sample monitoring wells to ensure that water quality standards are not exceeded at the boundary of a zone of discharge established by that specific condition and authorized by Rule 17-28.700(4)(a), Florida Administrative Code. A groundwater monitoring plan has been developed by the Applicant, with accompanying hydrogeological survey as mandated by Rule 17-28.700, Florida Administrative Code. The proposed groundwater monitoring system consists of 42 monitoring wells in and around the area of the proposed Class I and Class III landfill sites. The system is designed to monitor upgradient and downgradient flows in wells constructed to sample from the shallow and intermediate zone and from the deep zone (to some extent) on the east boundary of the Class I disposal site. Specific condition number 18 of the Notice of Intent to grant the permit and draft permit, to which the Applicant has agreed, requires that a detailed chemical characterization of a representative sample of leachate be performed, so as to allow for any necessary modifications to the list of chemical substances to be analyzed in water samples drawn from the monitoring wells on a quarterly basis. Although there are up-gradient monitoring wells for the shallow and intermediate portions of the surficial aquifer, there are no upgradient monitoring wells for the deep zone of the surficial aquifer. There are no upgradient monitoring wells on the west side of the landfill in the deep zone. The deep zone of the surficial aquifer is the zone between the intermediate zone and the top of the Hawthorn confining bed. The rock aquifer is present beneath the proposed landfill site and was encountered at well locations B-7, B-8, B-12 and B-14. That rock aquifer is hydrologically connected to and part of the deep zone, which is hydrogeologically connected throughout the site to the uppermost portions of the surficial aquifer lying beneath the landfill. The rock aquifer is a significant source of drinking water in Duval County and the surrounding northeast Florida area and is used as a supply source for domestic and commercial wells within one and one-half miles of the landfill Class I site. "Sinkers" are immiscible liquids contained in landfill leachate that are denser than water. When released from the landfill they would sink to the first low permeability unit in the surficial aquifer. This would be at the bottom of the surficial aquifer at the rock unit. Once they encountered a lower permeability unit or strata, sinkers would then move in a more lateral direction downgradient in undetermined directions. The silty clay layer depicted on Figure 9 of TRL Exhibit 51 would intercept those sinkers and cause them to tend to move in a direction toward the silty clay layer intercepted by well B-1. At that point the sinkers would then have a tendency to move in a north or south direction on top of the confining zone. The direction those sinkers would move, following a gradient, cannot be determined at present from the groundwater monitoring plan because no deep wells are proposed in either of those areas which could detect sinkers. The groundwater monitoring plan is thus not adequate for the deep zone or to detect pollutants that could migrate off site in the rock aquifer because there are no monitoring wells in the deep zone on the west, north and south sides of the Class I landfill area. Monitoring for sinker compounds in the deep zones is thus insufficient and water supply wells nearby in the deep zone would be at risk because there is no way to detect pollutants between those water supply wells and the source of the pollutants at the landfill. The groundwater monitoring plan is inadequate because there is insufficient information to determine the direction of water flow in the deep zone. Sufficient upgradient monitoring wells in the deep zone are necessary in order to determine the direction of water flow in the deep zone which will in turn indicate where additional deep zone monitoring wells should be located to detect contaminants migrating off site. Leachates also contain contaminant constituents or compounds called "floaters." Floaters are immiscible liquids which are lighter or less dense than water. They tend to float on top of the groundwater table. The hydrologic information depicted with the application and the Applicant's evidence is not sufficient to determine where floaters might migrate. The shallow monitoring wells referenced in TRL Exhibit 42 would not adequately detect floaters at or near the water table surface. Due to the lower lying stream or wetland systems on the north and south side of the Class I landfill on Trail Ridge, groundwater flows in the vicinity of those areas are likely moving northward and southward to some extent. Thus, TRL Exhibit 51, and particularly Figure 14 of that exhibit, is insufficient to support a determination of where monitoring wells should be located because it does not include the impact of the stream or wetland systems on the north and south sides of the landfill. Groundwater contours bend into the stream areas on the north and south sides of the landfill which would indicate groundwater flow to the south and the north instead of just from west to east. The general shape of these contour lines would resemble the contour lines depicted in Figure 16 of TRL Exhibit 51. These contour lines bend back to the east and the west on the north and south sides of the Class I landfill. Since there is groundwater flow to the north and to the south from the Class I landfill, intermediate and deep monitoring wells in addition to shallow wells, should be located along the west, north and south sides of the landfill. Because they are not in the groundwater monitoring plan thus far, the plan is inadequate. A grant of the permits should be conditioned on such additional wells being installed and made a part of the monitoring program, in accordance with the above findings. A zone of discharge for the proposed landfill has been established pursuant to Rule 17-28.700(4)(a)2., Florida Administrative Code, which is intended to extend vertically from the base of the surficial aquifer and horizontally 100 feet beyond the footprint of the landfill or to the compliance groundwater monitoring wells, whichever is less. (See pages 611- 618 of the transcript.) Therefore, even if the groundwater monitoring wells are closer than 100 feet to the footprint of the landfill, they are to be used for monitoring for compliance with applicable water quality standards, including the primary and secondary drinking water standards for G-II groundwater, as contained in Rules 17-550.310 and 17-550.320, Florida Administrative Code. The Applicant has agreed to this location of the wells, their spatial relationship to the footprint of the landfill, to the zone of discharge and to their use for compliance purposes. Storm Water and Surface Water Management System The Applicant proposes as part of its permit application a storm water discharge and surface water management system. The application for permitting for that system was submitted to the DER which reviewed it using the Water Management District's permitting criteria set forth in Chapters 40C-4 and 40C- 42, Florida Administrative Code. Pursuant to its independent permitting authority set forth in Section 373.413, Florida Statutes, the DER noticed its intent to issue the MSSW permit to the Applicant, based upon its opinion that the project will comply with applicable rules. The proposed storm water discharge/surface water management system (MSSW system) will utilize roadside swales, perimeter ditches, catch basins, culverts, detention ponds and pump stations to manage storm water in compliance with Chapters 17-25, 40C-4 and 40C-42, Florida Administrative Code. The solid waste disposal areas will operate as watersheds, routing storm water in to the MSSW system. The retention areas have been designed to handle the retention treatment requirements of a 25-year, 24-hour "design storm" runoff, resulting from approximately eight to nine inches of rainfall. The system is comprised of three independent parts; the Class I landfill system, the Class III landfill system and the separate roadway surface water management system. The Class I system will use temporary berms to intercept storm water runoff from the cap cover system of the landfill, on top of the solid waste disposal area. These top berms will divert the storm water runoff to regularly spaced pipes which will convey the storm water into the perimeter swale located at the foot of the landfill side slopes. The runoff will then be diverted through a culvert into a concrete-lined perimeter ditch which will convey it to the pond. The top berms of the landfill also operate as erosion control features, capturing and channelling some storm water runoff away from the side slopes of the landfill, thereby assisting in erosion control. The Class I retention pond covers an area of approximately ten acres and will contain approximately 43 million gallons of water at design water levels. The peak flow of storm water runoff from a design 25-year, 24-hour storm can be accumulated and released at predetermined rates. The runoff from the first one inch of rainfall in a 72 hour period is retained and stored in the pond. No discharge will be allowed to the pond's outfall system, rather all the outfall from the runoff from the first inch of rainfall will be routed through the sand filter system prior to discharge. When storm water runoff enters the pond, it will mix with the water already in the pond and become part of the total water column. When a rainfall event then produces greater than one inch of rainfall, some water will have to be discharged from the pond by passing it through the sand filter and then discharging through the outfall structure. The water discharged is water which was already resident in the pond before the rainfall event, mixed with the current rainfall runoff from that hypothetical rainfall event. The volume of the pond is so large that storm water runoff will constitute a very small fraction of the actual water volume in the pond at any given time. On the average, it will take 33 days for a given molecule of storm water runoff to travel through the pond, the sand filter and then be discharged through the outfall system. the sand filter system operates on a water level trigger device involving floats in wet wells attached to electrical switching mechanisms. When a certain water elevation in the wet wells, reflective of the elevation in the pond, is reached, the pumps automatically start and pump water into the filter chambers, causing the water to flow over a filtering sand. The filter will be maintained periodically by lowering of the water level to permit removal and replacement of the top six inches of sand in the filter. The Class III storm water pond is similar in design to the Class I pond except that it will not use a top berm. Rather, a perimeter swale will function similarly to the Class I landfill top berm, intercepting storm water runoff from the top and side slopes of the Class III landfill. The Class III storm water pond is equipped with the same type of filtration and pumping system as the Class I pond. The Class III system is designed also to retain the first inch of storm water runoff from a "design storm" rainfall in a 72 hour period. All of that runoff from the first inch of rainfall will likewise be routed through sand filtering prior to discharge. The roadway storm water system utilizes grassed roadside swales to act as a retention structure to filter the storm water runoff. The runoff retained in the swales will be conveyed by pipe to a smaller detention and dispersion pond located between the Class I and Class III disposal areas and built with the same design constraints as the Class I pond. The roadway system will not use a pumping system to operate, but rather discharge will occur through natural action of gravity through the dispersion pond. The filtered storm water runoff from the Class I and Class III disposal areas will be discharged into adjacent wetlands after it leaves the ponds. The discharge will be performed by a wetland irrigation system. The irrigation system will discharge the filtered storm water through conveyance pipes to the wetland boundaries. There a series of perforated pipes will extend outward from the conveyance pipes themselves and serve as a means of gradually releasing the filtered storm water into the wet land area as a means of wetland replenishment and mitigation. Concerning the issue of surface water quality, it has been established that the sand filtering systems on the Class I and Class III storm water ponds are capable of providing 100 percent of the treatment required by State water quality standards when considered in conjunction with the treatment capability of the ponds themselves as natural lake systems. The individual sand filters each provide twice the capacity for treatment necessary which equates to a safety factor of 2. With both filters operating, there is a combined safety factor of 4. Although the Class I and Class III retention ponds are designed with filtration systems, the primary pollution removal system will be the ponds themselves operating as natural lakes. Once storm water enters the ponds, the average residence time is adequate to allow the biological processes of uptake and assimilation to function to remove the bulk of the pollutants, including those derived from any spillage of leachate into the storm water management system and ultimately deposited into the ponds. The volatile organic compounds which can occur in the leachate can largely be removed simply by the process of evaporation, due to the adequate retention time of any leachate- containing storm water which reaches the ponds. It has been established that, due to the storm water pond's natural treatment mechanisms, especially the long retention time, the size and volume of the ponds, as well as the vegetated sides of the ponds, that, considering also the operation of the filter system, the water discharging from the Class I and Class III storm water treatment facility will have very low concentrations of total nitrogen, phosphorous, biochemical oxygen demand (BOD), suspended solids and heavy metals. The Applicant's expert witness on water quality and water chemistry, Dr. Harper, also assumed that the Class I retention pond would have some leachate migration into the pond through groundwater influx. Worst case scenarios were used to estimate this possible influx and the results established a maximum deposition of 2.46 gallons of leachate into the pond over a 65 day period. This amount would be diluted by a factor of 14 million solely by new storm water runoff and rain normally expected under average rainfall conditions during such a 65 day period, without even considering the considerable dilution by the existing water volume of approximately 43 million gallons already in the pond in such a period. Dr. Harper's testimony is accepted. It is unlikely that any runoff can enter the retention pond on one day and then exit within one day's time through the outfall overflow device. Even assuming that runoff occurs in excess of the designed one inch, that runoff would dilute with the large volume of water already present in the storm water pond. Thus, the new storm water would be mixed, diluted and subject to natural biological processes and the process of evaporation (of volatile organic compounds), operative in the pond before it can be released through the outfall structure. The runoff will enter the pond at the west end and discharge through the opposite or east end of the pond. The majority of water caused to be discharged through the outfall because of a larger-than-design storm event runoff would thus actually be water already present in the pond as opposed to incoming runoff from the recent rain event being deposited in the west end of the pond where the storm water system discharges from the Class I disposal area. Even a rainfall event producing twice the designed-for volume would produce no effect on the water quality of the discharge. Further, along with the filter systems and the natural processes of biological uptake, assimilation as well as evaporation in the natural lake system which would operate in the pond, the side slopes of both ponds will be vegetated so as to further assist in uptake and removal of any pollutants present in the runoff, further mitigating any potential for water quality impacts. It has been established that the surface water management system is designed to segregate surface water from leachate by minimizing the size of the landfill working face and reducing the potential for storm water to contact waste and become leachate. Further, a berm will be constructed around each working face which will encompass the entire active cell of the landfill, causing any runoff water entering the working face to remain there and percolate through the landfill to the leachate collection system, rather than entering the storm water system. If a severe rainfall event could cause leachate to overflow those berms, the design includes additional berms on the interior slopes of the landfill to catch that overflow and divert it back through the leachate collection system. The berms are relocated as the working face of the landfill changes, so they will continue to fulfill these functions on an ongoing basis. In terms of a worst case event, the Applicant has also established that the estimated impact of runoff from approximately one acre of exposed solid waste entering the retention pond would still cause no water quality impacts. Further assurance of leachate segregation from surface waters is provided in a spillage control plan which would be activated in the event of leachate spillage from a tanker truck. In connection with this, any grant of the permit should be conditioned upon an adequate berm system surrounding the tank truck leachate filling device in order to contain any such spill to prevent the leachate from entering the storm water retention facilities and surface waters. Such a system should also be characterized by (and the permit conditioned upon) retention berms or other forms of containment being placed around each leachate storage tank, designed to retain the full capacity of such a leachate storage tank in the event of a catastrophic tank valve, piping or other failure. It has been demonstrated, moreover, that if the leachate-storm water separation and control system were to fail in some way so that leachate directly entered the retention pond, the volume of leachate entering the pond would have to exceed approximately 150,000 gallons to cause any water quality violation in the storm water retention pond, even assuming the high concentration of contaminants in the leachate envisioned in the opinion of Dr. Robert Livingston, the Petitioners' aquatic ecologist and toxicologist. He raised concerns that pollution of the head water systems of the St. Johns and St. Mary's Rivers might result from the operation of the project. The Applicant has rebutted the concerns expressed by Dr. Livingston and Dr. Parks and established reasonable assurances that toxins and contaminants occurring in leachate will not deposit in surface waters of the State in any significant or rule-violative amounts for the reasons expressed in the above Findings of Fact. Draw-Down Effects The Petitioners contend that there will be a draw-down of groundwater levels in surrounding wetlands caused by these storm water ponds and associated pumping, in violation of the Water Management District's rules and policy embodied in MSSW Handbook Section 10.6.3. This section presumes an adverse impact on wetlands will result if the system causes the groundwater table to be lowered more than five feet lower than the average dry season low water table. The Petitioners' expert in this area, Dr. Motz, estimated that a measurable draw-down of groundwater of one to two feet in the wetlands water table would extend outward as far as maybe 1,000 feet in all directions from each of the storm water ponds. Dr. Motz used a large error convergence factor in his calculations, however, and also used a model for a confined aquifer, which was not shown to exist at the subject site. He did not use a model which should be appropriate for unconfined or semiconfined aquifers which the evidence reveals is the more appropriate hydrogeology which would be employed in groundwater modeling for the subject site. Dr. Motz' use of a large error convergence factor can potentially result in an answer which is far from the actual appropriate draw-down figure. Numerical models are approximations of reality and the smaller the error convergence factor, then the closer to the real number of the cone of depression, or draw-down level, the model will give. Consequently, the use of an analytical groundwater, cone of depression model was shown by the Applicants' witnesses to give a more accurate result, especially in view of the large error convergence factor employed by Dr. Motz in his numerical model. It was not shown that Dr. Motz had actually "calibrated" the groundwater model he employed. The Applicants' hydrogeology expert, Don Miller, used three analytical and two empirical methods to determine radius of influence or draw-down from the storm water ponds and calibrated the models he used. Validating the data or calibrating the model is a way of making sure the model actually represents the situation intended. Calibration is performed in this instance by inputting some data and then seeing if the model itself could accurately predict the remainder of the data of interest. Using these various methods, Dr. Miller arrived at a range of radius of influence likely to occur from the Class I storm water pond of 167 feet to 184 feet at the western end of the pond and approximately 40 feet at the eastern end. The maximum radius of influence for the Class III storm water pond was shown to be approximately 160 feet at the western end and 0 at the northeastern corner. The other hydrogeology expert for the Applicant, Dr. Leve, performed a separate analytical analysis of draw-down using the Southwest Florida Water Management District's "KOCH" model to produce a projected radius of influence of approximately 167 feet, which is comparable to the projections of Dr. Miller. In conjunction with this, it was shown that Dr. Motz' use of a small value for groundwater infiltration and the large error convergence factor served to increase his predicted radius of influence in an inaccurate way. Dr. Motz also used a higher value for transmissivity or hydraulic conductivity ("K"). The Applicant's experts relied on the average of the actual permeability test results obtained for the site. A different figure for transmissivity or hydraulic conductivity results from Dr. Motz taking into account two test wells in which hydraulic conductivity could not be measured because the well water level rose too quickly to obtain a measurement. Consequently, he predicted or assumed that that factor might affect the hydraulic conductivity at the site by a whole order of magnitude, which resulted in his 1,000 foot prediction for draw-down cone of influence. The problem here is that the evidence does not demonstrate clearly that this much- greater hydraulic conductivity factor with regard to these two wells, which was an isolated incident compared to all other wells tested, is not some mechanical or human error in the installation or evaluation of the wells. Further, even if one predicts the hydraulic conductivity of the unmeasured, apparently highly conductive wells at the geometric mean of all the hydraulic conductivity measurements for the water table zone (except for the marl zone) at 3.0 X 10 cm/sec or three times greater than the value used by the Applicant, it would result in a cone of influence of 265 feet instead of 184 feet. If one also assumed a value for the two ignored wells, as data points, by assuming that they had a hydraulic conductivity value of 3.5 x 10/-3 cm/sec, the highest reported well conductivity value, and then employed that in the empirical formula used by Donald Miller, it would still not greatly exceed the 265 foot cone of depression number. No evidence was adduced to demonstrate that a cone of depression of that magnitude would have any adverse affect on the wetlands, especially in view of the recharging of the wetlands through the storm water pumping and irrigation system. In summary, the totality of the evidence in the Applicant's case, especially on rebuttal, demonstrates that Dr. Motz' methodology significantly overestimated the radius of influence for draw-down at both storm water ponds. The parties agree that the maximum draw-down of 16 feet would occur within the Class I storm water pond, where a "seepage face" would be formed where the pond would cut into the water table through earth borrowing activities. The maximum draw-down inside the Class III storm water pond, where a seepage face would be formed by the excavation into the water table to construct the pond, will be 14 feet. The lowered groundwater within the storm water ponds is due in part to the natural sloping land surface of that area and the concurrent natural slope of the water level before the ponds are even excavated. The slope of draw-down will decrease rapidly, that is, much of the 14 foot or 16 foot apparent draw-down amount will be the result of the relatively sheer seepage face formed by the pond excavation. At the top of that seepage face, the groundwater cone of depression will flatten out considerably and very rapidly so that, as the slope of the draw-down decreases rapidly in the immediate vicinity of the pond, the groundwater outside the ponds themselves will actually be lowered less than five feet. The groundwater levels used in the application were based upon seasonal high water level for the site, rather than "average dry season low" water levels, as referenced in Section 10.6.3 of the Water Management District's Applicant's handbook. Therefore, the projected draw-downs are very conservative and would overestimate the actual draw-down for dry season low water table groundwater levels. Consequently, the weight of the evidence supports the Applicant's predictions on the effects of draw-down. The evidence demonstrates that draw-down from the storm water ponds associated with both landfills will have either no impact or minimal impact on wetland species, either transitional or submerged, in the surrounding wetlands. Silvi-culture activities on the site have considerably altered the area and lowered the natural water table through the construction of drainage structures by the timber company in the past. In general, the wetland jurisdictional lines from the storm water ponds are based on United States Army Corps of Engineers (Corps) wetland criteria and thus do not contain species generally considered to be wetland species for purposes of DER dredge and fill or Water Management District MSSW jurisdictional purposes. Many species used by the Corps in determining jurisdiction, such as slash pine, can grow both in uplands or wetlands. The edges of the areas delineated as jurisdictional wetlands are dominated by transitional and upland plant species such as slash pine, gallberry, palmetto, grapevine and huckleberry, which can tolerate dry conditions. It is only as one's investigation proceeds waterward or toward the center of the delineated wetlands, (in which area the land surface slopes down- gradient at the same area where the draw-down cone of influence rapidly diminishes to an insignificant level), that the plant species change to those species adapted to regular and periodic inundation for purposes of the State agencies' wetlands jurisdiction. The draw-down maximum for any wetland location using the maximum projected radius from Dr. Miller's efforts of 184 feet, (17 feet beyond the projection based upon the Water Management District's model), is on the southwest edge of the Class I pond. Maximum draw-down there will be 24' inches at the wetland boundary line, that is, the Corps jurisdictional boundary line where the dominant plant species are transitional or upland plants such as slash pine, gallberry and bay trees. Pine trees at this point exhibit tall and vigorous growth which indicates that the water table, before installation of the ponds, is already well below the surface, otherwise these upland trees would lack sufficient oxygen to grow if water levels were closer to the surface. The potential draw-down here would thus have little effect on this vegetation. There will be essentially no draw-down effect further down-gradient beyond the DER Water Management District jurisdictional boundary, where the pines are already of diminished stature because of water existing close to the land's surface and where DER wetland jurisdictionally-listed plants predominate. The draw-down at the wetland boundary line on the southeastern part of the Class I pond will be 9 2/3 inches. Wetland species which could be affected are found 50-60 feet beyond that radius of influence at this point. The radius of influence on the northern side of the Class I pond will not cross any wetland boundary until it widens at the northwestern corner. The maximum draw-down at the wet land line near the northwestern corner of the pond would be approximately 15 1/2 inches. Here again the predominant plant species are the upland species of slash pine and gallberry and thus the draw-down will have little effect on those species for reasons mentioned above. On the western edge of the Class III pond is an isolated wetland for purposes of the Water Management District MSSW and Corps jurisdiction only. The edge of that wetland is dominated by slash pine and gallberry. The estimated draw-down on the boundary line of that land in the area dominated by slash pine and gallberry is six inches. There will be no draw-down from that Class III borrow pond area in any wetland dominated by transitional or submerged species. In addition to the above considerations and factual findings concerning the effect of the draw-down, the Applicant is proposing an irrigation systems as delineated above, which will deliver water to the wetlands to mitigate and replenish any minimal impacts of groundwater draw-down. The irrigation system will increase the degree and duration of saturation of the soils at the wetlands' boundary. This will mitigate any minimal effect of draw- down and may actually have the effect of enhancing the health and quality of the wetlands over time, from the wetlands' boundary waterward. In order that the irrigation system will pose the maximum benefit and most closely imitate the natural systems, the irrigation system will be designed for flexible operation. A wetlands ecologist will review the wetlands quarterly and adjust the irrigation system as necessary, as to location and operational regime, in order to properly maintain the health, including water levels and hydro-periods in the wetlands. The Applicant has agreed that the grant of the permit be conditioned to allow for this ongoing quarterly investigation and adjustment. Dr. Motz indicated in his testimony his belief that, to a large extent, the water pumped to the wetlands through the irrigation system would simply immediately migrate to the groundwater and immediately back to the storm water pond, through the effects of the draw-down, and not serve the purpose of replenishing the wetlands. He admitted, however, that he did not know whether the proposed irrigation system would work or not. The Applicant's expert witness in this regard, Dr. Leve, established that the irrigation system would effectively distribute water into the wetlands and saturate the surface due to the "mound effect" of water at the irrigation systems' discharge point at the wetland boundary. He used a standard, generally-accepted "mounding model" to predict the effects of the mounding for the irrigation system. Mounding is a hydrogeological phenomenon whereby water will mound up and create a zone of saturation in the soil at the point of discharge to the ground surface. Mr. Leve ran that model for a cross-section of each of the storm water pumps. He also ran the model for two different values of groundwater inputs into the ponds. A figure of 28,800 gallons of groundwater infiltration into the pond per day, as predicted by the Applicant's expert witnesses, and the 100,000 gallon per day groundwater input predicted by Dr. Motz was used. For both cross- section locations examined by Dr. Leve, the discharge of 28,000 gallons per day at the wetland boundary would raise groundwater levels by approximately three inches. The discharge of 100,000 gallons per day at the same locations through the irrigation system would increase water levels by approximately nine inches. These calculations ware based upon the discharge of the groundwater inputs into the storm water pond only. Discharge additionally of the inputs from storm water runoff from the surface of the landfill into the pond and then through the irrigation system would also be delivered into the wetlands as warranted. Additionally, a berm system will prevent surface water runoff from entering the north dirt borrow area. A berm will be constructed at the eastern boundary of the north borrow area to maintain an interior water elevation of 125 feet or one foot above the natural ground, whichever is higher. Water levels will thus be maintained at the north borrow area so that there will be no lowering or de-watering of the groundwater table. Additionally, storm water will be diverted by berms along the west end of both the Class I and Class III landfills upgradient and into the wetlands, so that the adjoining wetlands receive significant surface water recharge that previously did not flow into those wetlands. Mitigation A mitigation plan was proposed for purposes of both the dredge and fill permit application and, in the solid waste landfill application, for the MSSW permitting. It was incorporated into the draft dredge and fill permit and draft landfill permit incorporated in the Department's Notice of Intent to issue. The mitigation plan and other measures will offset the impacts from filling and other activities caused by the project in both the dredge and fill and MSSW jurisdictional wetlands on the site. The proposed mitigation measures include the creation of 4.76 acres of new wetlands; the irrigation of the wetlands surrounding the Class I and Class III storm water ponds, as delineated above, and the diversion of surface water around the landfills into the wetlands to aid in their recharge. A high quality, forested wetland will be created utilizing the reliable method of mulching and, an extensive hardwood planting program which will include red maple, sweetgum, cypress and tupelo trees. The created wetland will contain deep water and transitional zones. The area will be monitored to insure 80 percent survival of the trees planted and routine maintenance will be performed. Approval of this mitigation plan and any issuance of the permits should include the requirement that rapid replanting be done to replace any dead trees and such approval should also be conditioned on the use of the largest trees possible to be planted, by appropriate tree planting equipment, so that the beneficial uptake and filtering functions, as well as wildlife habitat functions of such hardwood wetlands can begin operating as a mitigatory factor as soon as possible. The created wetland area will replace lost wetlands with a wetland type of higher quality and potentially higher habitat function, depending upon the maturity of the trees planted (see above condition). The wetland replacement ratio attendant to the creation of this wetland area is proposed to be 2.8:1 and the permit should be conditioned on at least that ratio being observed in the mitigation wetland installation plan. Although there was some testimony critical of the wetland creation proposal because it would alter 4.76 acres of uplands which might be of significance to the wildlife in the area, in fact the site of the mitigation area is currently pine plantation which has been greatly altered from its natural state. It does not currently provide high quality upland wildlife habitat. Additionally, only 30-40 percent of the uplands on the entire tract will be altered by the entire project construction proposed. This leaves a majority of the uplands presently on the site in their current condition to the extent that it serves as wildlife habitat at the present time. A conversion of the subject area into a high quality hardwood forest wetland, which would remain bordered by upland on one side in any event, will not have any significant impact on the present value of the mitigation areas as habitat. Wetlands Assessment and Impacts Through the use of consultant personnel skilled in the fields of surveying, biology and botany, the Applicant established jurisdictional lines demarcating the boundaries of DER jurisdiction for dredge and fill permitting purposes and MSSW permitting purposes in the field and adduced evidence of those boundaries at the hearing. The jurisdictional lines established were conservative in the sense that they reflect the jurisdictional standards of the U.S. Army Corps of Engineers, which is generally landward of the lines which would be established by the plant communities characteristic of DER dredge and fill and Water Management District MSSW jurisdiction. The locations of the flags as placed by the biology-botany consultant were then professionally surveyed and plotted by a trained surveyor such that the jurisdictional line was signed and sealed as a "specific purpose of survey." Further, a biologist met with the surveyors weekly to review the plotted line to ensure accuracy. That survey was submitted to the Department in connection with the applications herein. The Department supports that jurisdictional determination in this proceeding. The Department's own jurisdictional determination staff members were on the sites of the jurisdictional determinations for approximately eight days. The location of the wetland jurisdictional line for purposes of MSSW permitting has not been challenged by Petitioners, and no evidence regarding MSSW jurisdiction has been presented by Petitioners in this proceeding. The wetlands jurisdictional survey prepared by the Petitioners, however, showed "new" DER jurisdictional wetlands which would represent, if accepted, an alteration of the DER jurisdictional wetland boundary. Additionally, the challenge to the DER. jurisdictional determination is restricted by the Petitioners to the area around the Class I landfill footprint and its associated storm water pond. No evidence has been presented regarding the jurisdictional determination for the remainder of the site and project, including the access road. Witness Don Garlic has a degree in marine biology with additional coursework and training in the field of botany, including field training in wetland species. He visited the site for seven days for the purpose of critiquing the dredge and fill DER jurisdictional line established by the Applicant and offered as proof by the Applicant in this proceeding. In the 2-3 mile segment of the jurisdictional line around the Class I landfill and associated storm water pond, Mr. Garlick opined that there were three gaps 18-20 feet wide where he did not agree with the dredge and fill jurisdictional line determination. These areas represented by the gaps, if the gaps were determined to be jurisdictional, would add rather long, linear features of putative wetlands to the jurisdictional wetlands already encompassed by the proposed Class I portion of the project. They would add approximately 1/2 acre of additional DER jurisdictional wetlands impacted by the project. The Petitioners, however, did not establish the duration of water flow at any of the areas in which dredge and fill jurisdiction was contested. Mr. Garlick stated that water was flowing each of the seven days he was on the site, from March 28 to May 8, 1991, but stated that it was raining when he was there on April 23. He did not review rainfall data to determine whether it had rained prior to any of his visits. Likewise, he was not shown to have reviewed any groundwater data or to have performed any tests to ascertain groundwater levels in relation to claiming jurisdiction over the disputed Areas A, B, C and D depicted on Petitioners' Exhibit 8. This site has not experienced a prolonged drought. For the period 1988 through the hearing, only the latter portion of 1990 reflected a significant lack of rainfall based on rainfall data obtained from the National Oceanic and Atmospheric Administration Office (NOAA) at the U.S. Navy's nearby Cecil Field, as well as the Jacksonville International Airport. Nineteen eighty-eight, in fact, had above-average rainfall of 61 inches. The Class I landfill area was originally "flagged" in September and early October 1989. July, August and September 1989 were months of above average rainfall. September 1989 had 14 inches of rain, twice the normal rainfall. Nineteen ninety had slightly less than half of its average rainfall for the year, although it started out with normal rainfall and became dry in the fall months. There has since been twice the normal rainfall for the few months of 1991 prior to the hearing. A drought of the type and duration experienced in the latter part of 1990 would have had no significant effect on the plants at the sites in question (sites A, B, C and D). They are perennial plants that remain year-round and therefore are adapted to drought and flood conditions. (T-2047) 1/ The Applicant's jurisdictional determination based upon dominant plant species, established by its consultant in evidence was based upon perennial plant species. Therefore, the hydrological conditions on the site were normal ones when these areas were originally reviewed in 1989 and the jurisdictional delineations established and the conditions found at the site shortly prior to the hearing in March through early May 1991 by Mr. Garlick were unusually wet conditions and do not reflect the normal conditions prevailing at the site. Mr. Byron Peacock was accepted as an expert in wetlands ecology and botany with a B.S. degree in each of those disciplines, with emphasis on Florida wetland species, especially with regard to Florida fresh water wetlands. Mr. Peacock is quite familiar with the site, having been to the site "dozens of times" since September 1989, almost every month for a 21-month period. Mr. Godley, another of Applicant's expert witnesses, also visited the areas put into contention by Mr. Garlick in his testimony for purposes of testifying in rebuttal and also concluded that these areas were not jurisdictional for purposes of the DER's dredge and fill jurisdiction. Mr. Mike Eaton of DER visited at least one of the areas or sites in contention and was of the same opinion. Mr. Garlick had relied on flowing water being present and the plants present to determine that Area A, a ditch along Hells Bay Road, was a jurisdictional wetland area. The areas on both sides are upland. Mr. Garlick testified that there were breaks in the vegetation in Area A and that the vegetation was sufficient to establish a connection. Area A does not contain sufficient water to support a dominance of listed wetland species under either the "a or b tests," as provided in Rule 17-301.400(1)(a) and (b), Florida Administrative Code. There is upland vegetation growing all the way across the ditch on both sides at its connecting point and point of discharge to dredge and fill wetlands. If the ditch held water it would be wettest at this point of discharge into the jurisdictional wetlands, but the ditch does not contain water on a regular and periodic basis, as established by the testimony of Mr. Peacock. Therefore, the water observed in the ditch by Mr. Garlick would have been surface water runoff from the recent high rainfall. Concerning Area B in the Class I storm water pond footprint, Mr. Garlick indicated that he relied on herbaceous wetland plants as a basis for his finding of that as a jurisdictional area. He used the "b test" vegetation method of at least 80 percent transitional plants, less than 10 percent submerged or upland species, as well as the presence of "other indicators" of regular and periodic inundation for that Area B for purposes of the rule cited last above. Area B is a logging road and lies between upland stands of planted pines. It has been used as a road within the past year and there are "rutted- out" or gouged areas in the road caused by vehicular traffic which have puddled water, but between the puddles are areas dominated by upland vegetation. There is also a clear vegetative break in jurisdiction at the point where Area B connects to the jurisdictional line at Area B's southern end. The vegetation at that connecting point is a mixture of red. root, a transitional plant and many upland species, the dominant one being amphicarpum muhlenbergianum, which looks similar to red root in the field. Mr. Garlick testified that red root was the predominant plant in Area B. Mr. Garlick may have mistaken amphicarpum muhlenberqianum for red root. He was not familiar with that upland species and did not know if it was found at the site. A review of photographs from the 1950s, 1960s, 1970s and 1980s showed that Area B had historically always been uplands. The evidence shows that this area holds water only in limited areas following rainfall and that there is no hydrological, "a or b test" vegetative connection between these areas and jurisdictional waters of the State. Area C, located on the west side of the present West Fiftone Road, also contains part of an old road bed, as well as a ditch. Area C was determined to be within MSSW jurisdiction by the Applicant, but was also claimed as a dredge and fill jurisdictional area by Mr. Garlick for the Petitioner. Mr. Garlick indicated in his testimony that plants in Area C were mixed transitional and submerged species, but were sufficient to make out the area as within DER jurisdiction, based upon those plants. He also testified that different parts of Area C met the "a test" or the "b test." The ditch on the eastern side of Area C is dominated by upland vegetation, including amphicarpum grass, slash pine and goldenrod. The slash pines growing in the ditch, as shown by a photograph in evidence, were several years old. This ditch was dry on all of Mr. Peacock's visits to the site except recently during heavy rains. The remainder of Area C is characterized by a canopy of slash pines, a subcanopy of titi shrub of an upland type, with less than ten percent of the vegetation being characterized by bay and tupelos. There is a ground cover over most of that area consisting of upland species such as chokeberry, gallberry and reindeer moss. This area was determined to be jurisdictional for MSSW purposes because of a wet area in the middle containing fetter bush and sweet gallberry, which are both transitional species for jurisdictional purposes. The entire Area C was delineated as MSSW in the permit application, even though it may not all be jurisdictional, simply for ease of delineation and survey. The MSSW wetland areas within Area C, however, have no vegetative or hydrologic connection to the dredge and fill jurisdictional wetlands. Area C thus does not contain sufficient water or vegetation under either the A or B test connected with other jurisdictional areas to be considered jurisdictional for purposes of the DER's dredge and fill jurisdiction. Area D consists of a rutted trail-road used on a regular basis by persons visiting the tract. There is an upland pine plantation on either side of the roadway. Mr. Garlick contended there was a "flow way" in Area D, but that the vegetation was spotty or sporadic. During the past 21 months, Area D was dry every time Mr. Peacock was on the site, except recently after prolonged, heavy rains. At the eastern end of Area D near its connection to Area C, there is a patch of upland amphicarpum grass, growing all the way across the ditch and road. There is also the presence of beak rush, an upland plant which looks similar to submerged rush. There is insufficient water or wetland vegetation under either the a or b test to establish that this Area D is jurisdictional. The evidence thus did not support the Petitioner's contention that additional dredge and fill wetlands would be impacted by the project. The areas claimed by the Petitioners as additional jurisdictional wetlands did not contain sufficient water to be determined jurisdictional, pursuant to DER Rule 17-301, Florida Administrative Code. These areas held water only at certain times of the year in direct response to heavy or frequent rainfall and were normally influenced, that is, fed, by surface water rather than groundwater. Likewise, these areas did not contain sufficient plant species in the canopy, subcanopy or ground cover to be considered jurisdictional pursuant to vegetation indices and procedures delineated in Rule 17- 301.400(1)(a) or (b), Florida Administrative Code. Mr. Mike Eaton of DER testified and established a 1990 DER policy embodied in a memorandum admitted into evidence explaining how the Department employs the above-cited rule for purposes of using hydric soils in making dredge and fill jurisdictional determinations. Both Mr. Eaton and the DER policy in evidence established that hydric soils are not used by the Department except as an indicator of regular and periodic inundation once "b test" vegetation has been determined to be present for purposes of the above rule. Mr. Garlick testified that he used hydric soils as a "back up" to jurisdictional determinations based upon hydrology and plants. He did not identify any area where his jurisdictional determination was based on soils alone. The Department policy memorandum in evidence emphasizes the importance, in jurisdictional determinations with hydric soils as an aid, of not merely determining whether the soil in question is hydric, but also of investigating the specific characteristics of the soil profile, which the Department maintains must be performed by a soils scientist. Mr. Carlisle, a soil scientist, visited the site and took samples of the areas indicated by Mr. Garlick. These locations were located in an approximate fashion by Mr. Garlick on Petitioner's Exhibit 8 at the hearing. Thirty-four of the 35 samples taken were determined to be hydiric by Dr. Carlisle. There are, however, breaks of up to approximately 525 feet between the hydric soils test findings in Areas A, B and D and yet the distance between one hydric and non-hydric soil test finding was shown to be approximately 50 feet. No soil samples were taken by Dr. Carlisle in Area C. These samples are found to provide an insufficient basis for determining the presence of hydric soils throughout Areas A-D. Additionally, Areas A-D did not contain areas of "b test" vegetation contiguous to other jurisdictional areas. Therefore, even if hydric soils had been present throughout these areas, these soils standing alone, without supporting "b test" vegetation, are insufficient to establish jurisdiction in the areas maintained to be so by Mr. Garlick. General Wetland Impacts This project will impact wetlands subject to the DER jurisdiction and which are jurisdictional for MSSW purposes under Chapter 40C-4, Florida Administrative Code, the rules of the St. Johns River Water Management District. Thus, a dredge and fill permit is required pursuant to Section 403.91 et seq., Florida Statutes, and DER Rule 17-312, Florida Administrative Code. Areas subject to DER dredge and fill jurisdiction and MSSW permitting jurisdiction are considered pursuant to DER Rules 17- 301 and 40C-4, Florida Administrative Code. The 1,288 acre site contains approximately 550 acres of wetland, much of which contains planted pines as well as some naturally occurring pines, as well as hardwood swamp, cypress and gum swamp, seepage slope, ditches and swales. Virtually all of the wetlands have been adversely affected in some way by the forestry practices which have occurred and are still occurring on the site. Most of the sloughs and natural flow-ways have been channelized. Ditching has drained the adjacent wetlands and significantly altered the hydrology of the entire wetland system on the site. The wetland known as Hells Bay Swamp, immediately east of the landfills, is currently being clear cut by the Gilman Paper Company. The 550 acres of wetlands are jurisdictional for either dredge and fill or MSSW purposes or both. Some 3.17 acres of MSSW wetlands will be impacted by project construction; 1.61 acres of these are also dredge and fill wetlands. The 1.61 acres of the impacted dredge and fill and MSSW wetlands consist of roadside ditches along the Hells Bay Road and a road on the north side of the Class I landfill. These roads are currently subject to logging traffic, which decreases the usage of the roadways and ditches by wildlife. Consequently, the master of species present and using these ditches is limited. In addition to the 1.61 acres of ditches, the impacted MSSW wetlands also include 0.16 acres of wetland ditches along the entrance road in proximity to dredge and fill wetlands, a 0.80 acre isolated cypress head wetland located within the footprint of the Class I landfill and a 0.60 acre wetland located along West Fiftone Road extending into the south border of the Class I landfill footprint. The 0.80 acre cypress head has already been impacted by a logging road or fire break, and ditches have been constructed through the interior of it. The larger cypresses have been logged, and the remaining vegetation is sparse, rendering it of little quality as habitat for fish and wildlife. The 0.60 acre wetland extending into the south border of the Class I landfill is an old road bed with evidence of ruts from vehicular traffic depicted on photographs in evidence. This area has a slash pine canopy and is dominated by titi shrubs, with a few black gum and traditional wetland plant species such as fetter bush and gallberry in disconnected areas. It is a low quality wetland of scant value as habitat for fish or wildlife. Prior to and during construction, as a condition on a grant of the permits, all wetlands on the site will be protected from erosion, siltation, scouring or excessive deposition of turbidity, de-watering or other construction and operationally-related impacts by the installation and use of siltation barriers placed at wetland boundaries. Because of the significant possibility of the impacts mentioned above, especially siltation and turbidity, to the wetlands during the construction phase of the facilities and attendant to ultimate operation of the landfill itself, grant of the permit should be conditioned on acceptance of monthly inspections by DER enforcement personnel once construction has begun. Wildlife and Archaeological Resource Impacts Wildlife surveys were conducted by expert witness Isaac Rhodes Robinson and members of his staff, as well as by Biological Research Associates, Inc. in the months preceding the hearing. Mr. Robinson and the biologists on his staff spent approximately 1,000 man hours surveying the site, and Mr. Robinson, accepted as an expert in wildlife ecology and wetland ecology, testified on behalf of the Applicant in this proceeding. Assessments of the site were performed by reviewing relevant literature as well as conducting field surveys for both upland and wetland species. No evidence was found of any threatened or endangered species on the site. Mr. Robinson and his staff conducted surveys in 1990 and in early 1991 and biologists from Mr. Robinson's staff were present on the site at various times from September 1989 through the time of the hearing. Surveys performed by Mr. Robinson and his personnel were conducted in accordance with Florida Game and Fresh Water Fish Commission (FGFWFC) guidelines and exceeded that agency's guidelines by surveying 100 percent of the upland areas. No testimony of any witness in this proceeding indicated any physical evidence of use of the site by any endangered or threatened species. Wildlife surveys revealed a shall colony of gopher tortoises, listed as a species of special concern by the FGFWFC in a marginal habitat zone on the extreme western boundary of the Class I disposal area. The colony consists of less than ten individuals and there will not be a significant impact to the tortoises because the individuals will be trapped and relocated to a more suitable habitat on another area of he Applicant's tract, which will be undisturbed by the landfill or its operations, or else to a suitable habitat area off-site, as directed by the FGFWFC. Jay Stephen Godley was accepted as an expert in wildlife ecology and wetlands ecology. He directed an independent assessment of the site and project's impacts. The assessment included reviewing permitting documents, aerial photographs and literature pertaining to wildlife use of the site, as well as over 90 man hours spent at the site. He confirmed that the small population of gopher tortoises was the only significant species on the site and that the project would not significantly impact any listed wildlife species. Extensive trapping and investigation of gopher tortoise and armadillo burrows reveal no evidence of listed "commensal" species, or those species commonly found in association with gopher tortoises, such as Florida mice, gopher frogs, Florida pine snakes, or Eastern indigo snakes. In additions the isolated cypress head in the Class I landfill footprint was sampled for gopher frog tadpoles, and none were found. Florida pine snakes prefer scrub or sand hill habitats, neither of which are found on the site. Pine flatwoods environments, without the presence of either sand hill or scrub habitat, like this site, are not good indigo snake habitat. No indigo snakes' shed skins or other evidence of indigo snake frequency were observed on the site. Indigo snakes are large black snakes which are active during daylight hours and easy to observe in the course of extensive surveys such as those that were conducted for purposes of this project. Considering the amount of time spent by the various biologists on the site, it is quite likely that indigo snakes would have been observed if they frequented this site. The project will have no significant impact on wading birds. All wetlands were surveyed for listed bird species for a minimum of five days using FGFWFC guidelines. No wading birds were observed on the site during the 21 month period of review by Mr. Robinson's firm. The existence of the wood stork, bald eagle or Florida sand hill crane was not established on this site and is considered unlikely by the expert witnesses, whose opinions are accepted. No eagle nests were observed and, since the tree cover provides very limited extent of open water, the site is less than satisfactory as habitat for the little blue heron, snowy egret and Louisiana heron. The only wading bird observed by the Petitioner's expert witness on wildlife issues was a little blue heron observed in a wetland area east of the site, which is off the site being purchased by the Applicant and which was recently clear-cut by the Gilman Paper Company. The project will have no significant adverse impact on the Florida black bear's habitat. The black bear is a threatened species, but black bears do not use the site. No evidence was presented that black bears have ever been present on or in the immediate vicinity of the site. No witness, including Mr. Goodowns, an employee of Gilman Paper Company who has frequently visited and worked on this site over many years, has ever observed a black bear or any sign of a black bear present on the site. Bee hives have been kept at the site since at least 1969 and, although these are very attractive to black bears, they have never been known to have disturbed the hives, nor has it ever been necessary for bee keepers to erect electric fences or other devices to protect the hives from bears. The site presently is not far isolated from human activity, which fact deters the use of it as a habitat or an occasional travel way for black bears. It is located in an area completely enclosed by I-10, State Roads 228 and U.S. Highway 301, all heavily traveled public highways, as well as in close proximity to the town of Maxville, approximately two miles away, and Macclenny, approximately five miles away. Highways with high traffic volumes are significant barriers to movements of black bears, rendering it even less likely that black bears have or will frequent the site. The only evidence of potential black bear presence anywhere near the site presented by the Petitioners was the site's position near the Osceola Black Bear Range, as interpreted from one published article, as well as indication of three bear road kills from six to 15 miles away from the site, and supposed black bear movements recorded by the FGFWFC, all represented on a hand-drawn map, only admitted a corroborative hearsay pursuant to Section 120.58, Florida Statutes. The map exhibit contained the expert's own redrawing of his interpretation of the extent of the Osceola Black Bear Range from the article he referenced, which itself was not offered into evidence. Bear movements depicted on the map really consisted of those of a bear apprehended by the FGFWF and released in the area. The map did not show any roads, therefore making location and distances to the reported road kills speculative at best. Because black bears do not use this site and because of its encirclement by significant human activity, the site is not significant as a bear dispersal corridor or travelway between the Osceola Forest bear population and the Ocala Forest population. No direct evidence by radio-telemetry data or otherwise was offered to show that black bears actually move between the Osceola and Ocala Forest populations, nor particularly that they move through the area in the immediate vicinity of the project site. Construction of the landfill would not prevent the movement or foraging of black bears through the site. Neither fencing nor presence of traffic on the landfill access roads only during daylight hours would prevent such movement. It is also unlikely that bears would likely be hit by traffic on the roads because the noisy trucks which will use the road would provide ample warning to bear's of any danger from traffic so they would avoid it. If the landfill were constructed on this site, less than one-half of 5/100 of one percent of the 3,800 square- mile area of the Osceola Black Bear Range, referenced by the Petitioners' expert witness, would be impacted. The site itself does not provide high quality black bear' foraging or denning habitat. Even the Petitioners' expert characterized it as "good" or "better than average" habitat. All but 3.17 acres of the area to be impacted by the project is upland, consisting primarily of pine flatwoods. Authoritative studies show that flatwoods are not heavily utilized by bears, which spend 70 percent of their time in swamp or wetland habitat. The 550 acres of wetlands, including approximately 280 acres of swamps, which will be left undisturbed on the site, will provide habitat and travel corridors for the black bears should any ever frequent the site. Additionally, the 4.76 acres of hardwood wetlands to be created as mitigation, would add high quality wetland habitat for black bears. Therefore, due to the extremely small area involved, the unlikelihood of use by black bears and the mitigation proposed, the landfill will have virtually no impact on black bear habitat, travelways or populations. The evidence thus established that the project will not have an adverse impact on endangered or threatened species or their habitats. Because the site has been under extensive commercial forest management and harvest operations for over forty years, the density of plant and animal life has been reduced, thus making the site as a whole, low quality wildlife habitat.
Recommendation Having considered the foregoing Findings of Fact, Conclusions of Law, the evidence of record, the candor and demeanor of the witnesses and the pleadings and arguments of the parties, it is, therefore RECOMMENDED: That a Final Order be entered by the Department of Environmental Regulation approving Trail Ridge Landfill, Inc.'s applications for the above-referenced permits for the proposed solid waste management facility, including a solid waste management facility permit, a storm water/management and storage of surface waters permit and a dredge and fill permit, provided those mandatory conditions specified in the Notices of Intent to issue such permits, as well as those conditions found to be necessary in the above Findings of Fact and Conclusions of Law are made mandatory conditions of permitting and subsequent facility operations. DONE AND ENTERED this 20th day of September, 1991, in Tallahassee, Leon County, Florida. P. MICHAEL RUFF Hearing Officer Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, FL 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 20th day of September 1991.
The Issue The issue for disposition in this proceeding is whether, as alleged in an administrative complaint dated February 20, 1998, Respondent Craig J. Evans committed negligence in the practice of engineering when he erroneously determined that a real property parcel was not within the flood protection zone. If that violation occurred, an appropriate penalty must be recommended.
Findings Of Fact Respondent Craig J. Evans is and has been at all material times a professional engineer licensed in the State of Florida with license no. PE 0033652. He is currently practicing as a professional engineer, and is licensed as such, in St. Croix, U.S. Virgin Islands. In the approximate 15 years that Mr. Evans has been licensed as a professional engineer, the instant proceeding is the first disciplinary action or allegation of professional wrong-doing. In October 1992, Mr. Evans was engineer of record for a residence being built for his father on a parcel now designated as 1588 Chadwick Way, Tallahassee, Florida. On or about October 10, 1992, Mr. Evans signed and sealed a Leon County Flood Protection Certification for the Chadwick parcel in Killearn Lakes, Unit 3, Lot 3, Block B M. This certification was a necessary component of the local permitting process. In the certification Mr. Evans stated that the parcel was at or above the flood protection elevation. After the certificate was filed and the building permit was issued, Fred Varn, then a Leon County building inspector, spoke to Mr. Evans about the inspector's concern that the floor level of the house might be too low. Mr. Varn was aware that some other properties in the area had flooded. Mr. Evans responded that he felt the level was safe, but he was willing to listen and he raised the floor level approximately 16 inches. The house was built and Mr. Evans and his parents lived in it for a short time. It rained during that time and according to Mr. Evans, there was a little bit of flooding on the front of the property and a little of standing water in the back, but neither lasted long. Mr. Evans' parents put the Chadwick house on the market and Mr. and Mrs. George Simonof expressed an interest in purchasing it. In response to the Simonof's surveyor's concerns about flooding, Mr. Evans or his father faxed the October 10, 1992, certification to the Simonofs on June 30, 1994. The Simonofs, in turn, provided the certification to their surveyor and lender. On July 14, 1994, the Simonofs closed on their purchase of the Chadwick house. In early October 1994, Tallahassee experienced severe rainstorms. Between October 6-12, 1994, the Simonof's property on Chadwick flooded. With the help of friends and neighbors, they filled sandbags and placed them around the house. The house did not flood but the backyard was filled with standing water. Contrary to Mr. Evans' certificate, the property on Chadwick is within the flood protection zone. When he determined the location of the flood zone, Mr. Evans scaled from Federal Emergency Management Area (FEMA) maps to a plat map showing the lot's location. He erred in the plotting process, a common error, but one that a prudent engineer would be more careful to avoid. Initially, the Chadwick property appeared to Mr. Evans to be in the flood zone, so he rechecked his work by pulling certificates on two lots nearby and found they were not certified in the flood zone either. He was somewhat familiar with the property as he used to jog in the Killearn area. He had no personal knowledge of flooding there prior to his certification. Mr. Evans did not exercise due care in preparing his flood zone certification and was negligent in the practice of engineering. If he had checked his plotting, he would have realized there should have been more distance between his 2100 and 1600 feet lines. Further, in close cases, a survey should have been obtained. It was not sufficient that Mr. Evans attempted to check his work against two certifications of other lots in the area; he did not know the engineers who did the work and could not be certain of their certificates' relevance or accuracy. He did not speak with other property owners in the area nor did he seek information from Leon County staff who would be familiar with flooding problems. To Mr. Evans' credit he raised the house elevation upon query by the building inspector and the house did not flood. However, the buyers of the property relied on his erroneous certificate and suffered some loss due to the flooding.
Recommendation Based on the foregoing, it is hereby RECOMMENDED: that the Board of Engineers issue its Final Order finding Craig Evans guilty of negligence and assessing a fine of $750. DONE AND ENTERED this 30th day of December, 1998, in Tallahassee, Leon County, Florida. MARY CLARK Administrative Law Judge Division of Administrative Hearings The DeSoto Building 1230 Apalachee Parkway Tallahassee, Florida 32399-3060 (850) 488-9675 SUNCOM 278-9675 Fax Filing (850) 921-6847 Filed with the Clerk of the Division of Administrative Hearings this 30th day of December, 1998. COPIES FURNISHED: Natalie A. Lowe, Esquire Department of Business and Professional Regulation Board of Professional Engineers 1208 Hays Street Tallahassee, Florida 32301-0750 Dennis Barton, Executive Director Board of Professional Engineers Department of Business and Professional Regulation Northwood Centre 1940 North Monroe Street Tallahassee, Florida 32399 Lynda L. Goodgame, General Counsel Department of Business and Professional Regulation Northwood Centre 1940 North Monroe Street Tallahassee, Florida 32399-0792 E. Renee Alsobrook, Esquire Post Office Box 10426 Tallahassee, Florida 32302-0426
Findings Of Fact Charlotte Highlands is an approximately 97-acre mobile home subdivision in Charlotte County, Florida. The roads in the subdivision are unpaved. The stormwater sheet flow in the area is from west to east. To the east of Charlotte Highlands is a 21-acre hardwood swamp, the wetlands in question in this proceeding. Stormwater from the 97-acre subdivision west of the wetlands and from the 250 acres west of the subdivision flows to the east into the wetlands. Water flows out of the wetlands to the east, from the 21-acre wetlands through a stream into Myrtle Slough. Myrtle Slough is part of the waters of the State. The County wishes to create a stormwater drainage system for Charlotte Highlands. Under the County's plan, stormwater from the 97-acre subdivision would be discharged into the wetlands owned by Desrosiers Brothers. Although the County and the Department view this project as involving only the discharge of stormwater from the 97-acre subdivision into the wetlands, the stormwater discharged would include the stormwater flowing into the 97-acre subdivision from the 250 acres located directly west of the subdivision. The County met with individuals from the Southwest Florida Water Management District, and that agency questioned the method of calculations used by the County in determining the amount of runoff into the proposed drainage system. Although new calculations of stormwater runoff volume were performed by the County, those new calculations were not provided to the Department in the County's permit application. The wetlands in question contain cypress, maples, laurel oak, bay trees, percia, dahoon holly, buttonbush, ferns, palmetto, and wet pine. Some of these species, especially the maples, cannot withstand much flooding. The outflow from the wetland into Myrtle Slough is via a natural stream. Although there are some indications that some excavation may have taken place in the stream, such as the spoil located near the cattle watering pond near the mouth of the wetlands, water flows from the wetlands to Myrtle Slough through a natural watercourse with no man-made connections. The hydroperiod is the length of time water stays in a wetlands before it drains out of the wetlands. This determines the water level, the critical factor affecting a wetland's ability to perform its vital functions. If the rate or volume of either the inflow or outflow of a wetlands is altered enough, the water level changes, usually with adverse environmental consequences. Certain species of flora will die off if the water level rises too much. Others require high water levels for their survival. In order to assess the effects of a proposed alteration to such a system, one must determine the existing high pool and low pool. Donald H. Ross established the high and low pools for the County. He went to the wetlands and observed the stain, rack, and lichen lines on tree trunks. He also observed the cypress buttress. Ross also determined the invert of the stream, the elevation at which water first starts to run in it. Based solely on this site visit, the County determined the high pool in the wetlands to be at 14.8 NGVD and the low pool to be at 14.1 NGVD. No rainfall data was collected and analyzed; no hydrological studies were performed; no observations were made over a period of time. There are two aspects of this project which can alter the hydroperiod of the wetlands. The first involves the amount of water entering the wetlands, and the second involves the amount of water leaving the wetlands. Currently, runoff from the 97-acre subdivision as well as the 250-acre area west of the subdivision drains toward the wetlands. The County intends to pave the roads in the subdivision and construct a system of swales. Although the paving will increase the impervious surface by an insignificant amount, the runoff will be delivered to the wetlands faster. Accordingly, peaks in water level will occur more suddenly with increased water arriving more quickly. Stormwatr is discharged into wetlands to take advantage of the pollutant-filtering functions of wetlands vegetation. To realize this function, the water must be held in the wetlands for a certain amount of time. The County intends to accomplish this by the installation of a control structure, known as a weir, which will regulate the amount of water leaving the wetlands. The County proposes to construct a weir on the stream between the wetlands and Myrtle Slough approximately 100 feet from the mouth of the wetlands. The top of the weir for this system will be set at 14.8 NGVD, the high pool established by Ross for the County. The weir will also have an orifice set at 14.1 NGVD, the low pool established by Ross and the County, which will allow a constant flow of water out of the wetlands at that elevation. The control structure will cause water to remain in the wetlands for a longer period of time, which will raise the water level in the wetlands by some amount. In order to accurately predict this amount, it is necessary to determine the storage capacity of the wetlands. The County calculated that a storage capacity of 177,761 cubic feet would be required for the wetlands to contain the first one-half inch of rainfall from the 97-acre subdivision. No calculations have been made as to the storage capacity required for the wetlands to contain the first one inch of rainfall from the 97-acre subdivision as well as the 250-acre area that drains into the subdivision which then drains toward the wetlands. The County has failed to establish the hydroperiod of the wetlands. Having failed to establish the hydroperiod of the wetlands, the impact of its project on the wetlands cannot be determined. As an alternative to this project the County considered rerouting the stormwater away from the wetlands. Diverting necessary water from the wetlands would result in the desiccation of the wetlands. However, an increased water flow if not properly discharged would likely result in an over impoundment of the wetlands. Either approach would have an adverse impact on a productive wetland system, such as the wetlands involved here, and a change in the vegetation would adversely impact the wetland's ability to treat the discharge. The treatment of stormwater in wetlands is a relatively new technique. Although some projects have been approved in other parts of the State, projects such as that proposed by the County have not been used yet in southwest Florida.
Recommendation Based upon the foregoing Findings of Fact and Conclusions of Law, it is, RECOMMENDED that a Final Order be entered denying Charlotte County's application for a wetlands stormwater discharge facility permit. DONE and RECOMMENDED this 8th day of October, 1987, at Tallahassee, Florida. LINDA M. RIGOT, Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32399-1550 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 8th day of October, 1987. APPENDIX TO RECOMMENDED ORDER, CASE NO. 87-0243 Although Charlotte County filed a document called Proposed Findings of Fact and Conclusions on the Evidence, rather than setting forth any findings of fact the County simply makes what it calls a Comparison of Evidence on Issue 1 and a Comparison of Evidence on Issue 2, listing under each heading excerpts from the testimony of each of the witnesses in this proceeding. Accordingly, no rulings are made herein on Charlotte County's proposed findings of fact since it is determined that there are none. Desrosiers Brothers' proposed findings of fact numbered 1-9, 15, 17, 24, 26, 27, and 38 have been adopted either verbatim or in substance in this Recommended Order. Desrosiers Brothers' proposed findings of fact numbered 10-12, 19-21, 23, 25, 29-37, 40, and 41 have been rejected as not constituting findings of fact but rather as constituting argument of counsel or recitations of the testimony. Desrosiers Brothers' proposed findings of fact numbered 13, 14, 16, 18, 22, 28, and 39 have been rejected as being unnecessary or subordinate to the issues under consideration herein. The Department's proposed findings of fact numbered 1, 2, 14 in part, 15, 16 in part, 17 in part, 18-22, 27, and 28 in part have been adopted either verbatim or in substance in this Recommended Order. The Department's proposed findings of fact numbered 5 and 6 have been rejected as not constituting findings of fact but rather as constituting argument of counsel or recitations of the testimony. The Department's proposed findings of fact numbered 16 in part, and 17 in part have been rejected as being unnecessary or subordinate to the issues under consideration herein. The Department's proposed findings of fact numbered 3, 4, and 7-13 have been rejected as being contrary to the weight of the evidence in this cause. The Department's proposed findings of fact numbered 14 in part, 23-26, and 28 in part have been rejected as not being supported by the evidence in this cause. COPIES FURNISHED: Dale Twachtmann, Secretary Department of Environmental Regulation 2600 Blairstone Road Tallahassee, Florida 32399-2400 Philip J. Jones, Esquire 201 West Marion Avenue Suite 301 Punta Gorda, Florida 33950 Matthew G. Minter, Esquire 18500 Murdock Circle Port Charlotte, Florida 33948-1094 Richard Grosso, Esquire Department of Environmental Regulation 2600 Blairstone Road Tallahassee, Florida 32399-2400 =================================================================
Findings Of Fact Description of Proposed Fill Project DER proposes to deny three alternative proposals to fill all or part of Petitioners' real property located in Key West, Florida. The property is rectangular, approximately three acres in size, with 300 feet bordering Roosevelt Boulevard (High-Way A1A) to the south and approximately 300 feet bordering Key West International Airport to the north. The easterly property line is 489.4 feet and the westerly line is 434.63 feet. The Straits of Florida (Atlantic Ocean) are immediately on the other side of Roosevelt Boulevard to the south. The property has a strip of approximately 90 feet of upland and transitional wetland adjacent to Roosevelt Boulevard, with the rest of the property being covered by a salt pond of approximately 40 acres in size (Jnt. Ex. 1). Petitioners initially submitted a permit application in July, 1983, to fill the entire property for construction of multifamily housing units. On May 4, 1984, after discussion with a DER permitting official, Petitioners submitted a second application containing two alternative, less extensive development proposals. The first alternative involves the placement of fill over a 300' x 230' area (approximately 9722 cubic yards) extending 230 feet from the property along Roosevelt Boulevard out into the water. This alternative would entail construction of 24 family housing units, consisting of six basic structures, each four-stories high. The second alternative involves subdividing the property into six separate lots connected by a central fill road with cul-de- sac. Each lot, approximately .4 acres in size, would contain a single family house on pilings and an associated fill pad for parking. The fill pads would be connected to a approximately 300' x 30' entrance road constructed on fill material. Presumably, this second alternative would contain the same amount of total fill as required in the first. As it presently exists, the salt pond (a part of which applicant would fill) serves several significant and beneficial environmental functions. In regard to water quality, the pond stores, filters, and purifies large quantities of storm water which drain from the airport and South Roosevelt Boulevard. The filling of any portion of this pond would diminish this capacity. (Jnt. Ex. 1) Because of their relatively isolated nature, the organic detrital material that is produced from the leaf litter of fringing mangroves is broken down into a very fine and readily usable form by bacteria. As a result, when there is an occasional exchange between the salt pond and tidal waters, the exported organics are in a very desirable form for higher trophic levels in the food web such as small fish, crustaceans, filter feeders, and various larval forms of marine life. (Jnt. Ex. 1) The salt pond proper provides valuable habitat for fish and wildlife, most notable of which are avifauna. The pond has apparently become established as a healthy, self-sustaining ecosystem providing permanent and temporary food, shelter and refuge for many faunal species which play significant and necessary ecological roles both in the salt ponds and other tidal and brackish water systems. (Jnt. Ex. 1) Through the placement of fill and the displacement of present salt pond habitat, water quality and the biological resources in the immediate and surrounding areas would be expected to undergo degradation. (Jnt. Ex. 1) Through the encroachment of development in this area, which presently lacks residential development, biological integrity standards would be expected to fall below acceptable levels. The proposed fill areas would reduce wind- driven circulation in the pond so as to stress levels of oxygen, salinity, temperature and turbidity. Runoff from the proposed fill would introduce nutrients and elevate turbidity during storm events. Finally, elevated turbidity levels could be expected during the actual filling process and the various species of fish and wildlife now located over the project site would be temporarily disturbed by construction activities and permanently displaced in the long term through the loss of habitat. (Jnt. Ex. 1) There is a 40' zoning setback and another 50' easement owned by the City of Key West, which together form a 90' strip on the property adjacent to Roosevelt Boulevard. This 90-foot strip is largely upland and some transitional wetland. There is no zoning impediment to any of the development alternatives proposed by Petitioners. The property is currently zoned R2H (multifamily residential) by the City of Key West. II. DER's Action on the Application After DER received and reviewed Petitioners initial application on July 22, 1983, a completeness summary was sent on August 17, 1983, requesting additional information. DER received the additional information on March 23, 1984, after which it notified Petitioners that additional information was needed. Petitioners met with DER officials on April 20, 1984, and submitted additional information on May 4, 1984, including the two alternative proposals. DER issued the "Intent to Deny" all three of the proposed projects on July 19, 1984 (Jnt. Ex. 1). On May 16, 1984, a DER Environmental Specialist visited the site of the proposed projects and conducted a biological and water quality assessment. This assessment was later submitted, in report form, as the Permit Application Appraisal, dated June 7, 1984. This appraisal, uncontested by Petitioners, indicates that each of the three fill proposals would take place in waters of the state and result in water quality violations under Rules 17-3.051(1), 17- 3.061(2)(c), (j) and (r); 17-3.121(7), (13) and (28); Chapter 17-4, Florida Administrative Code; and Chapter 403, Florida Statutes. Water quality problems associated with the project were identified as diminished storm water treatment, reduced beneficial deterital material, stress on oxygen levels, salinity, temperature, and turbidity, and an introduction of nutrients. (Jnt. Ex. 1) Although a DER dredge and fill permitting official testified that any filling of the salt pond would be detrimental to the birds and animals which feed there on a daily basis, and that, in his view, a "substantial amount" of filling would not be allowed by DER, there are development projects (other than the three presented by Petitioners) which, in his view, may qualify for a permit under DER rules. DER has, in the past, issued permits authorizing the construction of above-ground residences over wetland properties. Under DER's permitting standards, one or more single-family residences could be built on the property if the structures were built on stilts, did not violate water quality standards, had acceptable drainage, and did not result in adverse storm water discharges. In evaluating such an application, any mitigation an applicant could provide, such as enhancing flushing in the salt ponds by the installation of a culvert to open water, would be balanced against any adverse impacts expected from the filling activity. The three alternative filling proposals submitted by Petitioners (including drawings and designs) do not, however as yet, fall within or satisfy these general perimeters of permitting acceptability.
Recommendation Based on the foregoing, it is RECOMMENDED: That Petitioners' application to fill (containing three alternative proposals) be denied for failure to prove compliance with applicable permitting standards contained in Chapter 403, Florida Statutes, and Chapters 17-3 and 17- 4, Florida Administrative Code. DONE and ORDERED this 26th day of July, 1985, in Tallahassee, Florida. R. L. CALEEN, JR. Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 26th day of July, 1985.
Findings Of Fact Upon consideration of the oral and documentary evidence in the record, as well as the pleadings and joint prehearing stipulation, the following relevant facts are found: Cast-Crete owns and operates a concrete batch plant in Hillsborough County, Florida, and manufactures concrete products such as reinforced beams, lintels, seals and drainage structures on the property. The plant is located on the west side of State Road 579, 3/4 mile north of Interstate 4, Section 28, Township 28 South, Range 20 East. The concrete products are manufactured in various forms which are laid out over a large portion of Cast-Crete's property. Lubricating oils are utilized to facilitate the removal of the product from the confining forms. During this process some of the lubricating oil is spilled onto the ground. Also, cleaning solutions containing degreasers are utilized to wash the concrete trucks eight to ten times per day. This solution ends up on the ground. Aggregate limerock (crushed limestone) is used in the concrete formulation process and is stored in large piles on the property. In order to contain the dust, water is sprayed on the aggregate piles 24 hours a day. The wash water from the continuous process of wetting the aggregate, other waste water and some stormwater is channeled through the property and into a settling pond in the northwest corner of Cast-Crete's property. This pond discharges continuously off the property by way of a concrete flume into a county maintained ditch. Water in the ditch travels in a westerly direction approximately 200 to 300 yards before it passes under Black Dairy Road, where the watercourse deepens and widens. The ditch discharges into a marshy area which drains into Six Mile Creek and other water bodies. The pond at the northwest corner of Cast-Crete's property is equipped with a metal skimming device to remove oils and greases floating on the surface of the pond. Nevertheless, it is estimated that approximately 100 gallons of oil per year are discharged by Cast-Crete. Oil and grease in the outflow water is occasionally above 5 mg/L. Oil and grease layers have been observed on water at both Black Dairy Road and Six Mile Creek, probably resulting from road run- off. Approximately 90 percent of the water discharged from the property is a result of the wetting or washdown of the aggregate piles. The excess water which comes from the aggregate piles is laden with dissolved limestone, lime and limestone particles. This limestone dust raises the pH level of the water. Because of the continued wetting of the aggregate, water flows through the settling ponds and off of Cast-Crete's property at a rate of approximately 4.8 gallons per minute, or 7,200 gallons per day or 2.5 million gallons per year. During a rain event, the flow increases markedly. Except during times of heavy rainfall, water flowing from the respondent's property provides a thin stream of water in the drainage ditch approximately six inches wide and several inches deep. The pH of the wastewater from Cast-Crete's discharge flume is between 10 and 11 units. During high volume flows, the pH remains at or above 11 units. An increase of one unit of pH in the wastewater means that the wastewater has become 10 times more basic, since pH is measured on a logarithmic scale. The natural background of unaffected streams in the area of and in the same watershed as the Cast-Crete property is less than 8.5 units. Specific conductance or conductivity is the measure of free ions in the water. Typical conductivity readings from other water bodies in Hillsborough County range between 50 and 330 micromhos per centimeter. The specific conductance of Cast-Crete's wastewater ranges from 898 to 2000 micromhos per centimeter. This is due to the presence of calcium carbonate and calcium hydroxide in the water. Blue-green algae is the dominant plant species in the ditch between the Cast-Crete discharge flume and the first 150 meters of the ditch. A biological survey of the ditch system indicates that the diversity of species east of Black Dairy Road is low. This is attributable in part to the high pH of the wastewater. The low diversity can also be attributed to the fact that the County maintains the ditch by use of a dragline on an annual basis. Background samples from a site within one mile to the northwest of the Cast-Crete property were taken. The site (a stream passing under Williams Road) is an appropriate place to take background samples because the water there is unaffected by Cast-Crete's discharge or other man-induced conditions. The pH background sample ranged from 4.6 units to 5.1 units. The specific conductance background samples ranged from 70 to 100 micromhos per centimeter. Samples taken from a site potentially impacted by Cast-Crete's discharge showed a pH level of from 6.35 to 7.37 units and specific conductance of from 592 to 670 micromhos per centimeter. Cast-Crete discharges water from its concrete plants operation without a permit from the DER.
Recommendation Based upon the findings of fact and conclusions of law recited herein, it is RECOMMENDED that a Final Order be entered requiring respondent to submit a complete application for an industrial wastewater permit within thirty (30) days, and that, if it fails to do so, it cease discharging wastewater from its property until such time as an appropriately valid permit is issued by the DER. Respectfully submitted and entered this 3rd day of May, 1985, in Tallahassee, Florida. DIANE D. TREMOR Hearing Officer Division of Administrative Hearings The Oakland Building 2009 Apalachee Parkway Tallahassee, Florida 32301 (904) 488-9675 Filed with the Clerk of the Division of Administrative Hearings this 3rd day of May, 1985. COPIES FURNISHED: David K. Thulman Assistant General Counsel Department of Environmental Regulation Twin Towers Office Building Blairstone Road Tallahassee, FL 32301 W. DeHart Ayala, Jr. 501 E. Jackson Street Suite 200 Tampa, FL 33602 Victoria Tschinkel Secretary Department of Environmental Regulation Twin Towers Office Building 2600 Blairstone Road Tallahassee, FL 32301 ================================================================= AGENCY FINAL ORDER ================================================================= STATE OF FLORIDA DEPARTMENT OF ENVIRONMENTAL REGULATION DEPARTMENT OF ENVIRONMENTAL REGULATION, STATE OF FLORIDA, Petitioner, vs. CASE NO. 84-1647 CAST-CRETE CORPORATION OF FLORIDA Respondent. /
